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Falls Creek — vertical structure, 0–3 days

The shape of the modelled column above this mountain: temperature and wet-bulb against height, humidity beside it, and four restrained readings of what that shape is. Up to nine requested pressure levels, sparse and terrain-filtered, not a sounding — /now has the surface observations, which are measurements and are deliberately kept separate from this.

VIC · lifted 1500–1780 m

Model
View
Humidity
Wed 30 12:00

12 valid times, 6-hourly AEST, out to 72 hours. Hours between these are not drawn.

ECMWF IFS · run Tue 29 2200hrs AEST · 1200Z · 13 h ago · fetched 9 min ago · valid Wed 30 12:00 AEST · model grid terrain 1129 m

ECMWF IFS · run Tue 29 2200hrs AEST · 1200Z · 13 h ago · fetched 9 min ago · valid Wed 30 18:00 AEST · model grid terrain 1129 m

ECMWF IFS · run Tue 29 2200hrs AEST · 1200Z · 13 h ago · fetched 9 min ago · valid Thu 1 00:00 AEST · model grid terrain 1129 m

ECMWF IFS · run Tue 29 2200hrs AEST · 1200Z · 13 h ago · fetched 9 min ago · valid Thu 1 06:00 AEST · model grid terrain 1129 m

ECMWF IFS · run Tue 29 2200hrs AEST · 1200Z · 13 h ago · fetched 9 min ago · valid Thu 1 12:00 AEST · model grid terrain 1129 m

ECMWF IFS · run Tue 29 2200hrs AEST · 1200Z · 13 h ago · fetched 9 min ago · valid Thu 1 18:00 AEST · model grid terrain 1129 m

ECMWF IFS · run Tue 29 2200hrs AEST · 1200Z · 13 h ago · fetched 9 min ago · valid Fri 2 00:00 AEST · model grid terrain 1129 m

ECMWF IFS · run Tue 29 2200hrs AEST · 1200Z · 13 h ago · fetched 9 min ago · valid Fri 2 06:00 AEST · model grid terrain 1129 m

ECMWF IFS · run Tue 29 2200hrs AEST · 1200Z · 13 h ago · fetched 9 min ago · valid Fri 2 12:00 AEST · model grid terrain 1129 m

ECMWF IFS · run Tue 29 2200hrs AEST · 1200Z · 13 h ago · fetched 9 min ago · valid Fri 2 18:00 AEST · model grid terrain 1129 m

ECMWF IFS · run Tue 29 2200hrs AEST · 1200Z · 13 h ago · fetched 9 min ago · valid Sat 3 00:00 AEST · model grid terrain 1129 m

ECMWF IFS · run Tue 29 2200hrs AEST · 1200Z · 13 h ago · fetched 9 min ago · valid Sat 3 06:00 AEST · model grid terrain 1129 m

ECMWF AIFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Wed 30 12:00 AEST · model grid terrain 1129 m Incomplete — some of this run is missing. Drawn values are genuine; gaps are not zeroes. Provider detail: missing variables: wind_gusts_10m.

ECMWF AIFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Wed 30 18:00 AEST · model grid terrain 1129 m Incomplete — some of this run is missing. Drawn values are genuine; gaps are not zeroes. Provider detail: missing variables: wind_gusts_10m.

ECMWF AIFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Thu 1 00:00 AEST · model grid terrain 1129 m Incomplete — some of this run is missing. Drawn values are genuine; gaps are not zeroes. Provider detail: missing variables: wind_gusts_10m.

ECMWF AIFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Thu 1 06:00 AEST · model grid terrain 1129 m Incomplete — some of this run is missing. Drawn values are genuine; gaps are not zeroes. Provider detail: missing variables: wind_gusts_10m.

ECMWF AIFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Thu 1 12:00 AEST · model grid terrain 1129 m Incomplete — some of this run is missing. Drawn values are genuine; gaps are not zeroes. Provider detail: missing variables: wind_gusts_10m.

ECMWF AIFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Thu 1 18:00 AEST · model grid terrain 1129 m Incomplete — some of this run is missing. Drawn values are genuine; gaps are not zeroes. Provider detail: missing variables: wind_gusts_10m.

ECMWF AIFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Fri 2 00:00 AEST · model grid terrain 1129 m Incomplete — some of this run is missing. Drawn values are genuine; gaps are not zeroes. Provider detail: missing variables: wind_gusts_10m.

ECMWF AIFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Fri 2 06:00 AEST · model grid terrain 1129 m Incomplete — some of this run is missing. Drawn values are genuine; gaps are not zeroes. Provider detail: missing variables: wind_gusts_10m.

ECMWF AIFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Fri 2 12:00 AEST · model grid terrain 1129 m Incomplete — some of this run is missing. Drawn values are genuine; gaps are not zeroes. Provider detail: missing variables: wind_gusts_10m.

ECMWF AIFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Fri 2 18:00 AEST · model grid terrain 1129 m Incomplete — some of this run is missing. Drawn values are genuine; gaps are not zeroes. Provider detail: missing variables: wind_gusts_10m.

ECMWF AIFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Sat 3 00:00 AEST · model grid terrain 1129 m Incomplete — some of this run is missing. Drawn values are genuine; gaps are not zeroes. Provider detail: missing variables: wind_gusts_10m.

ECMWF AIFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Sat 3 06:00 AEST · model grid terrain 1129 m Incomplete — some of this run is missing. Drawn values are genuine; gaps are not zeroes. Provider detail: missing variables: wind_gusts_10m.

GFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Wed 30 12:00 AEST · model grid terrain 1327 m

GFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Wed 30 18:00 AEST · model grid terrain 1327 m

GFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Thu 1 00:00 AEST · model grid terrain 1327 m

GFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Thu 1 06:00 AEST · model grid terrain 1327 m

GFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Thu 1 12:00 AEST · model grid terrain 1327 m

GFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Thu 1 18:00 AEST · model grid terrain 1327 m

GFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Fri 2 00:00 AEST · model grid terrain 1327 m

GFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Fri 2 06:00 AEST · model grid terrain 1327 m

GFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Fri 2 12:00 AEST · model grid terrain 1327 m

GFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Fri 2 18:00 AEST · model grid terrain 1327 m

GFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Sat 3 00:00 AEST · model grid terrain 1327 m

GFS · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Sat 3 06:00 AEST · model grid terrain 1327 m

ICON · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Wed 30 12:00 AEST · model grid terrain 1352 m

ICON · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Wed 30 18:00 AEST · model grid terrain 1352 m

ICON · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Thu 1 00:00 AEST · model grid terrain 1352 m

ICON · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Thu 1 06:00 AEST · model grid terrain 1352 m

ICON · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Thu 1 12:00 AEST · model grid terrain 1352 m

ICON · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Thu 1 18:00 AEST · model grid terrain 1352 m

ICON · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Fri 2 00:00 AEST · model grid terrain 1352 m

ICON · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Fri 2 06:00 AEST · model grid terrain 1352 m

ICON · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Fri 2 12:00 AEST · model grid terrain 1352 m

ICON · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Fri 2 18:00 AEST · model grid terrain 1352 m

ICON · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Sat 3 00:00 AEST · model grid terrain 1352 m

ICON · run Wed 30 0400hrs AEST · 1800Z · 7 h ago · fetched 9 min ago · valid Sat 3 06:00 AEST · model grid terrain 1352 m

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +8.3° base +6.5° top dry-bulb +12.4° base · +10.1° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer No measured depth No contiguous moist interval
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +8.4° base +6.8° top dry-bulb +12.4° base · +10.8° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer No measured depth No contiguous moist interval
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown 1 warm-layer inversion
Resort wet-bulb +9.1° base +7.6° top dry-bulb +11.6° base · +10.1° top
Moisture + DGZ 0.4 km+ 5393–5784 m+
Moist layer 2.6 km+ 3158–5784 m
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +8.4° base +7.0° top dry-bulb +10.6° base · +9.1° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer No measured depth No contiguous moist interval
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +9.2° base +7.5° top dry-bulb +10.7° base · +8.8° top
Moisture + DGZ 0.4 km+ 5335–5775 m+
Moist layer 4.2 km+ 1559–5775 m
Moist at resort Partial 221 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +9.0° base +7.4° top dry-bulb +12.9° base · +11.1° top
Moisture + DGZ 0.4 km+ 5326–5770 m+
Moist layer 2.6 km+ 3144–5770 m
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +9.0° base +7.5° top dry-bulb +11.3° base · +9.7° top
Moisture + DGZ 0.4 km+ 5330–5771 m+
Moist layer 2.6 km+ 3144–5771 m
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +8.9° base +7.4° top dry-bulb +9.9° base · +8.4° top
Moisture + DGZ 0.4 km+ 5386–5759 m+
Moist layer 4.6 km+ 1129–5759 m
Moist at resort Base to top 280 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +9.4° base +7.7° top dry-bulb +9.6° base · +7.9° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 3.2 km 1129–4351 m
Moist at resort Base to top 280 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +9.0° base +7.4° top dry-bulb +9.0° base · +7.5° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 2.0 km 1129–3125 m
Moist at resort Base to top 280 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +8.6° base +6.9° top dry-bulb +8.6° base · +7.1° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 2.0 km 1129–3123 m
Moist at resort Base to top 280 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +7.7° base +5.7° top dry-bulb +7.8° base · +6.3° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 0.4 km 1129–1524 m
Moist at resort Partial 24 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +8.7° base +6.8° top dry-bulb +12.2° base · +9.9° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer No measured depth No contiguous moist interval
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +9.5° base +7.6° top dry-bulb +13.8° base · +11.5° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer No measured depth No contiguous moist interval
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown 1 warm-layer inversion
Resort wet-bulb +9.1° base +7.7° top dry-bulb +12.6° base · +11.1° top
Moisture + DGZ 0.4 km+ 5373–5794 m+
Moist layer 2.6 km+ 3163–5794 m
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +8.4° base +7.1° top dry-bulb +11.3° base · +9.7° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer No measured depth No contiguous moist interval
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +8.8° base +7.1° top dry-bulb +11.9° base · +9.8° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 1.2 km 3157–4380 m
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +9.5° base +7.8° top dry-bulb +13.0° base · +11.0° top
Moisture + DGZ 0.4 km+ 5405–5778 m+
Moist layer 2.6 km+ 3148–5778 m
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +9.5° base +8.1° top dry-bulb +11.8° base · +10.2° top
Moisture + DGZ 0.4 km+ 5406–5779 m+
Moist layer 2.6 km+ 3149–5779 m
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +9.1° base +7.5° top dry-bulb +10.1° base · +8.5° top
Moisture + DGZ 0.4 km+ 5390–5763 m+
Moist layer 4.6 km+ 1129–5763 m
Moist at resort Base to top 280 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +8.9° base +7.3° top dry-bulb +9.6° base · +7.9° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 3.2 km 1129–4360 m
Moist at resort Base to top 280 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +8.8° base +7.1° top dry-bulb +9.3° base · +7.6° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 3.2 km 1129–4353 m
Moist at resort Base to top 280 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +8.2° base +6.6° top dry-bulb +8.6° base · +7.2° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 2.0 km 1129–3131 m
Moist at resort Base to top 280 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +8.1° base +6.4° top dry-bulb +8.5° base · +6.9° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 2.0 km 1129–3111 m
Moist at resort Base to top 280 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +7.7° base +5.7° top dry-bulb +12.5° base · +9.1° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer No measured depth No contiguous moist interval
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown 1 warm-layer inversion
Resort wet-bulb +8.3° base +7.1° top dry-bulb +12.1° base · +11.2° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer No measured depth No contiguous moist interval
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown 1 warm-layer inversion
Resort wet-bulb +8.8° base +7.5° top dry-bulb +10.7° base · +9.1° top
Moisture + DGZ 0.5 km+ 5268–5779 m+
Moist layer 3.7 km+ 2069–5779 m
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown 1 warm-layer inversion
Resort wet-bulb +8.0° base +7.0° top dry-bulb +10.6° base · +9.8° top
Moisture + DGZ 0.5 km+ 5288–5768 m+
Moist layer 2.6 km+ 3144–5768 m
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +8.7° base +7.3° top dry-bulb +10.7° base · +10.1° top
Moisture + DGZ 0.5 km+ 5297–5765 m+
Moist layer 2.6 km+ 3142–5765 m
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown 1 warm-layer inversion
Resort wet-bulb +8.9° base +7.7° top dry-bulb +13.6° base · +12.9° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 1.2 km 3132–4357 m
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +8.9° base +7.3° top dry-bulb +9.1° base · +7.4° top
Moisture + DGZ 0.4 km+ 5329–5757 m+
Moist layer 4.4 km+ 1327–5757 m
Moist at resort Base to top 280 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +9.0° base +7.5° top dry-bulb +9.0° base · +7.5° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 3.0 km 1327–4337 m
Moist at resort Base to top 280 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +5.2° base +4.1° top dry-bulb +5.5° base · +4.3° top
Moisture + DGZ 0.6 km+ 5132–5718 m+
Moist layer 4.4 km+ 1327–5718 m
Moist at resort Base to top 280 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown 1 warm-layer inversion
Resort wet-bulb +3.6° base +3.3° top dry-bulb +4.8° base · +4.9° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 0.2 km 1327–1531 m
Moist at resort Partial 31 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown 1 warm-layer inversion
Resort wet-bulb +4.7° base +3.5° top dry-bulb +5.6° base · +4.1° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 1.8 km 1327–3102 m
Moist at resort Base to top 280 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown 1 warm-layer inversion
Resort wet-bulb +5.2° base +3.8° top dry-bulb +6.1° base · +4.5° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 3.0 km 1327–4298 m
Moist at resort Base to top 280 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +8.6° base +6.6° top dry-bulb +12.8° base · +9.9° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer No measured depth No contiguous moist interval
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +8.8° base +7.2° top dry-bulb +12.7° base · +11.3° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer No measured depth No contiguous moist interval
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown 1 warm-layer inversion
Resort wet-bulb +9.3° base +8.3° top dry-bulb +12.5° base · +10.9° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 2.3 km 2066–4378 m
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown 1 warm-layer inversion
Resort wet-bulb +8.5° base +7.5° top dry-bulb +10.8° base · +9.4° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 2.3 km 2056–4368 m
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +7.9° base +6.3° top dry-bulb +10.1° base · +7.4° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 2.3 km 2052–4360 m
Moist at resort No overlap 0 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +8.9° base +7.7° top dry-bulb +10.1° base · +8.4° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 3.0 km 1352–4361 m
Moist at resort Base to top 280 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown 1 warm-layer inversion
Resort wet-bulb +9.1° base +7.9° top dry-bulb +9.7° base · +8.4° top
Moisture + DGZ 0.5 km+ 5277–5768 m+
Moist layer 4.4 km+ 1352–5768 m
Moist at resort Base to top 280 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +8.7° base +7.3° top dry-bulb +9.2° base · +7.7° top
Moisture + DGZ 0.5 km+ 5244–5754 m+
Moist layer 4.4 km+ 1352–5754 m
Moist at resort Base to top 280 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +4.4° base +3.7° top dry-bulb +4.8° base · +3.9° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 3.0 km 1352–4341 m
Moist at resort Base to top 280 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown 1 warm-layer inversion
Resort wet-bulb +5.1° base +4.9° top dry-bulb +5.2° base · +5.2° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 1.8 km 1352–3128 m
Moist at resort Base to top 280 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown 1 warm-layer inversion
Resort wet-bulb +5.6° base +5.1° top dry-bulb +5.6° base · +5.3° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 0.7 km 1352–2045 m
Moist at resort Base to top 280 m moist of 280 m resolvable

At this valid time

Full supplied profile, whichever chart view is shown No warm-layer inversion
Resort wet-bulb +5.8° base +4.6° top dry-bulb +5.8° base · +4.7° top
Moisture + DGZ No overlap Moisture and DGZ are vertically separate
Moist layer 1.7 km 1352–3096 m
Moist at resort Base to top 280 m moist of 280 m resolvable

Modelled vertical profile

Temperature, wet-bulb and relative humidity against metres above sea level

Full column · surface through the highest genuine supplied level.

Falls Creek — full column profile, 0–3 days Full column view for Falls Creek, from 900 to 5900 metres above sea level. The complete genuine profile is drawn through the highest supplied level. Two panels share the same linear vertical axis. The left panel plots the selected model's dry-bulb and wet-bulb temperature against height between -26 and 21 degrees Celsius, with a zero-degree reference, the model's own grid terrain shaded at its base, and the resort's lowest and highest lifted elevations marked. The right panel plots relative humidity on a fixed nought to one hundred per cent scale with the 80 per cent moist-layer threshold marked. Dots mark the pressure levels the model actually supplies, labelled in hectopascals on the right; the lines are straight interpolation between those levels and stop at the highest one supplied. Nothing is drawn above it. The humidity panel can be narrowed or hidden to give the temperature panel the width; that changes how wide each panel is drawn and nothing else — not the levels, the scales, or the diagnostics. 2000 4000 m -20 -10 0 10 20 -25 -15 -5 5 15 0 °C top 1780 m base 1500 m Temperature °C — dry-bulb and wet-bulb 0 25 50 75 100 80% Relative humidity % RH % hPa ECMWF IFS, valid Wed 30 12:00 model grid terrain 1129 m DGZ ≥ sfc 850 700 600 500 ECMWF IFS, valid Wed 30 18:00 model grid terrain 1129 m DGZ ≥ sfc 850 700 600 500 ECMWF IFS, valid Thu 1 00:00 model grid terrain 1129 m MOIST ≥ DGZ ≥ MOIST + DGZ MOIST ≥ sfc 850 700 600 500 ECMWF IFS, valid Thu 1 06:00 model grid terrain 1129 m DGZ ≥ sfc 850 700 600 500 ECMWF IFS, valid Thu 1 12:00 model grid terrain 1129 m MOIST ≥ DGZ ≥ MOIST + DGZ MOIST ≥ sfc 850 700 600 500 ECMWF IFS, valid Thu 1 18:00 model grid terrain 1129 m MOIST ≥ DGZ ≥ MOIST + DGZ MOIST ≥ sfc 850 700 600 500 ECMWF IFS, valid Fri 2 00:00 model grid terrain 1129 m MOIST ≥ DGZ ≥ MOIST + DGZ MOIST ≥ sfc 850 700 600 500 ECMWF IFS, valid Fri 2 06:00 model grid terrain 1129 m MOIST ≥ DGZ ≥ MOIST + DGZ MOIST ≥ sfc 850 700 600 500 ECMWF IFS, valid Fri 2 12:00 model grid terrain 1129 m MOIST DGZ ≥ MOIST sfc 850 700 600 500 ECMWF IFS, valid Fri 2 18:00 model grid terrain 1129 m MOIST DGZ ≥ MOIST sfc 850 700 600 500 ECMWF IFS, valid Sat 3 00:00 model grid terrain 1129 m MOIST DGZ ≥ MOIST sfc 850 700 600 500 ECMWF IFS, valid Sat 3 06:00 model grid terrain 1129 m MOIST DGZ ≥ MOIST sfc 850 700 600 500 ECMWF AIFS, valid Wed 30 12:00 model grid terrain 1129 m DGZ ≥ sfc 850 700 600 500 ECMWF AIFS, valid Wed 30 18:00 model grid terrain 1129 m DGZ ≥ sfc 850 700 600 500 ECMWF AIFS, valid Thu 1 00:00 model grid terrain 1129 m MOIST ≥ DGZ ≥ MOIST + DGZ MOIST ≥ sfc 850 700 600 500 ECMWF AIFS, valid Thu 1 06:00 model grid terrain 1129 m DGZ ≥ sfc 850 700 600 500 ECMWF AIFS, valid Thu 1 12:00 model grid terrain 1129 m MOIST DGZ ≥ MOIST sfc 850 700 600 500 ECMWF AIFS, valid Thu 1 18:00 model grid terrain 1129 m MOIST ≥ DGZ ≥ MOIST + DGZ MOIST ≥ sfc 850 700 600 500 ECMWF AIFS, valid Fri 2 00:00 model grid terrain 1129 m MOIST ≥ DGZ ≥ MOIST + DGZ MOIST ≥ sfc 850 700 600 500 ECMWF AIFS, valid Fri 2 06:00 model grid terrain 1129 m MOIST ≥ DGZ ≥ MOIST + DGZ MOIST ≥ sfc 850 700 600 500 ECMWF AIFS, valid Fri 2 12:00 model grid terrain 1129 m MOIST DGZ ≥ MOIST sfc 850 700 600 500 ECMWF AIFS, valid Fri 2 18:00 model grid terrain 1129 m MOIST DGZ ≥ MOIST sfc 850 700 600 500 ECMWF AIFS, valid Sat 3 00:00 model grid terrain 1129 m MOIST DGZ ≥ MOIST sfc 850 700 600 500 ECMWF AIFS, valid Sat 3 06:00 model grid terrain 1129 m MOIST DGZ ≥ MOIST sfc 850 700 600 500 GFS, valid Wed 30 12:00 model grid terrain 1327 m DGZ ≥ sfc 850 800 700 600 500 GFS, valid Wed 30 18:00 model grid terrain 1327 m DGZ ≥ sfc 850 800 700 600 500 GFS, valid Thu 1 00:00 model grid terrain 1327 m MOIST ≥ DGZ ≥ MOIST + DGZ MOIST ≥ sfc 850 800 700 600 500 GFS, valid Thu 1 06:00 model grid terrain 1327 m MOIST ≥ DGZ ≥ MOIST + DGZ MOIST ≥ sfc 850 800 700 600 500 GFS, valid Thu 1 12:00 model grid terrain 1327 m MOIST ≥ DGZ ≥ MOIST + DGZ MOIST ≥ sfc 850 800 700 600 500 GFS, valid Thu 1 18:00 model grid terrain 1327 m MOIST DGZ ≥ MOIST sfc 850 800 700 600 500 GFS, valid Fri 2 00:00 model grid terrain 1327 m MOIST ≥ DGZ ≥ MOIST + DGZ MOIST ≥ sfc 850 800 700 600 500 GFS, valid Fri 2 06:00 model grid terrain 1327 m MOIST DGZ ≥ MOIST sfc 850 800 700 600 500 GFS, valid Fri 2 12:00 model grid terrain 1327 m MOIST ≥ DGZ ≥ MOIST + DGZ MOIST ≥ sfc 850 800 700 600 500 GFS, valid Fri 2 18:00 model grid terrain 1327 m MOIST DGZ ≥ MOIST sfc 850 800 700 600 500 GFS, valid Sat 3 00:00 model grid terrain 1327 m MOIST DGZ MOIST sfc 850 800 700 600 500 GFS, valid Sat 3 06:00 model grid terrain 1327 m MOIST DGZ MOIST sfc 850 800 700 600 500 ICON, valid Wed 30 12:00 model grid terrain 1352 m DGZ ≥ sfc 850 800 700 600 500 ICON, valid Wed 30 18:00 model grid terrain 1352 m DGZ ≥ sfc 850 800 700 600 500 ICON, valid Thu 1 00:00 model grid terrain 1352 m MOIST DGZ ≥ MOIST sfc 850 800 700 600 500 ICON, valid Thu 1 06:00 model grid terrain 1352 m MOIST DGZ ≥ MOIST sfc 850 800 700 600 500 ICON, valid Thu 1 12:00 model grid terrain 1352 m MOIST DGZ ≥ MOIST sfc 850 800 700 600 500 ICON, valid Thu 1 18:00 model grid terrain 1352 m MOIST DGZ ≥ MOIST sfc 850 800 700 600 500 ICON, valid Fri 2 00:00 model grid terrain 1352 m MOIST ≥ DGZ ≥ MOIST + DGZ MOIST ≥ sfc 850 800 700 600 500 ICON, valid Fri 2 06:00 model grid terrain 1352 m MOIST ≥ DGZ ≥ MOIST + DGZ MOIST ≥ sfc 850 800 700 600 500 ICON, valid Fri 2 12:00 model grid terrain 1352 m MOIST DGZ ≥ MOIST sfc 850 800 700 600 500 ICON, valid Fri 2 18:00 model grid terrain 1352 m MOIST DGZ MOIST sfc 850 800 700 600 500 ICON, valid Sat 3 00:00 model grid terrain 1352 m MOIST DGZ MOIST sfc 850 800 700 600 500 ICON, valid Sat 3 06:00 model grid terrain 1352 m MOIST DGZ MOIST sfc 850 800 700 600 500

Dry-bulb Wet-bulb Relative humidity Resort elevation band Moist layer Moist + DGZ overlap Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — shaded Dendritic range −12 to −18 °C — shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — partly shaded Dendritic range −12 to −18 °C — shaded Dendritic range −12 to −18 °C — shaded Dendritic range −12 to −18 °C — shaded Modelled inversion layer Model grid terrain

Calculation method

Every level plotted here is the model’s own pressure-level temperature and humidity, taken from the same profile the snow level on the 3–7 day pages is derived from — the same builder, the same pressure-aware wet-bulb, and the same rule discarding levels that lie below the model’s own terrain. Nothing is recalculated for this page. This product requests 1000/925/850/700/600/500 hPa for ECMWF IFS and AIFS; GFS and ICON add 950/900/800. Unsupported or all-null triplets remain absent. Nothing is drawn or inferred beyond the highest genuine level supplied. Lines between two dots are straight interpolation between adjacent supplied levels and nothing more; at an alpine grid point those levels are routinely 1.5 km apart, so a real melting layer, cold pool or shallow inversion inside that gap is invisible here. Full column and Mountain detail are two linear display scales over these same levels and diagnostics; Mountain detail stops drawing above 700 hPa but does not recalculate or discard the complete profile. Moist depth uses a descriptive 80% relative-humidity threshold across adjacent supplied levels: it describes where the model is humid, and is not a cloud or snowfall detection. Dendritic-growth overlap is reported only where the supplied levels genuinely bracket -12 to -18 °C; where they stop warmer than that, the answer is “not covered by the supplied levels”, which is a statement about the data and not about the atmosphere. None of this is converted into a snowfall amount or a snow-quality score. Background

Weather data by Open-Meteo.com · ECMWF IFS — © ECMWF, licensed CC BY 4.0 · ECMWF AIFS — © ECMWF, licensed CC BY 4.0 · NOAA GFS — NOAA/NCEP, public domain · ICON — © Deutscher Wetterdienst, licensed CC BY 4.0

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5800 m (4671 m).
Lowest-layer lapse rate
14.6 °C/km between the model surface (1129 m) and 850 hPa (1573 m) — at or above the dry adiabatic rate. Measured across 444 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
No two adjacent supplied levels are both at or above 80% RH, so no depth can be measured. A single humid level is not a depth.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5535 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5792 m (4663 m).
Lowest-layer lapse rate
3.7 °C/km between the model surface (1129 m) and 850 hPa (1564 m) — stable — shallow fall with height. Measured across 435 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
No two adjacent supplied levels are both at or above 80% RH, so no depth can be measured. A single humid level is not a depth.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5419 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5784 m (4655 m).
Lowest-layer lapse rate
-0.7 °C/km between the model surface (1129 m) and 850 hPa (1562 m) — temperature rises with height. Measured across 433 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
  • 1129–1562 m (the model surface to 850 hPa): 11.3 °C rising to 11.6 °C, 0.7 °C/km of warming over 433 m.
A feature of this coarse model profile, not an observed inversion. It may equally be an artefact of interpolating a wide grid over steep terrain.
Moist-layer depth
2626 m contiguous at or above 80% RH, 3158–5784 m across 700 hPa, 600 hPa, 500 hPa (lowest 83%). The layer runs into the top of the supplied profile, so its real depth is at least this and unknown above it. Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5393 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5780 m (4651 m).
Lowest-layer lapse rate
1.2 °C/km between the model surface (1129 m) and 850 hPa (1554 m) — stable — shallow fall with height. Measured across 425 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
No two adjacent supplied levels are both at or above 80% RH, so no depth can be measured. A single humid level is not a depth.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5416 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5775 m (4646 m).
Lowest-layer lapse rate
10.5 °C/km between the model surface (1129 m) and 850 hPa (1559 m) — at or above the dry adiabatic rate. Measured across 430 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
4216 m contiguous at or above 80% RH, 1559–5775 m across 850 hPa, 700 hPa, 600 hPa, 500 hPa (lowest 83%). The layer runs into the top of the supplied profile, so its real depth is at least this and unknown above it. Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5335 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5770 m (4641 m).
Lowest-layer lapse rate
1.5 °C/km between the model surface (1129 m) and 850 hPa (1542 m) — stable — shallow fall with height. Measured across 413 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
2626 m contiguous at or above 80% RH, 3144–5770 m across 700 hPa, 600 hPa, 500 hPa (lowest 82%). The layer runs into the top of the supplied profile, so its real depth is at least this and unknown above it. Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5326 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5771 m (4642 m).
Lowest-layer lapse rate
1.7 °C/km between the model surface (1129 m) and 850 hPa (1551 m) — stable — shallow fall with height. Measured across 422 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
2627 m contiguous at or above 80% RH, 3144–5771 m across 700 hPa, 600 hPa, 500 hPa (lowest 93%). The layer runs into the top of the supplied profile, so its real depth is at least this and unknown above it. Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5330 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5759 m (4630 m).
Lowest-layer lapse rate
2.9 °C/km between the model surface (1129 m) and 850 hPa (1541 m) — stable — shallow fall with height. Measured across 412 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
4630 m contiguous at or above 80% RH, 1129–5759 m across the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa (lowest 87%). The layer runs into the top of the supplied profile, so its real depth is at least this and unknown above it. Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5386 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5755 m (4626 m).
Lowest-layer lapse rate
7.5 °C/km between the model surface (1129 m) and 850 hPa (1540 m) — steep. Measured across 411 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
3222 m contiguous at or above 80% RH, 1129–4351 m across the model surface, 850 hPa, 700 hPa, 600 hPa (lowest 84%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5303 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5746 m (4617 m).
Lowest-layer lapse rate
5.6 °C/km between the model surface (1129 m) and 850 hPa (1538 m) — moderate — near the saturated rate. Measured across 409 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
1996 m contiguous at or above 80% RH, 1129–3125 m across the model surface, 850 hPa, 700 hPa (lowest 93%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5174 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5734 m (4605 m).
Lowest-layer lapse rate
5.1 °C/km between the model surface (1129 m) and 850 hPa (1539 m) — moderate — near the saturated rate. Measured across 410 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
1994 m contiguous at or above 80% RH, 1129–3123 m across the model surface, 850 hPa, 700 hPa (lowest 83%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5014 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5705 m (4576 m).
Lowest-layer lapse rate
5.3 °C/km between the model surface (1129 m) and 850 hPa (1524 m) — moderate — near the saturated rate. Measured across 395 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
395 m contiguous at or above 80% RH, 1129–1524 m across the model surface, 850 hPa (lowest 99%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 4880 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5800 m (4671 m).
Lowest-layer lapse rate
15.4 °C/km between the model surface (1129 m) and 850 hPa (1577 m) — at or above the dry adiabatic rate. Measured across 448 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
No two adjacent supplied levels are both at or above 80% RH, so no depth can be measured. A single humid level is not a depth.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5569 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5794 m (4665 m).
Lowest-layer lapse rate
11.6 °C/km between the model surface (1129 m) and 850 hPa (1567 m) — at or above the dry adiabatic rate. Measured across 438 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
No two adjacent supplied levels are both at or above 80% RH, so no depth can be measured. A single humid level is not a depth.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5424 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5794 m (4665 m).
Lowest-layer lapse rate
-0.7 °C/km between the model surface (1129 m) and 850 hPa (1567 m) — temperature rises with height. Measured across 438 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
  • 1129–1567 m (the model surface to 850 hPa): 12.3 °C rising to 12.6 °C, 0.7 °C/km of warming over 438 m.
A feature of this coarse model profile, not an observed inversion. It may equally be an artefact of interpolating a wide grid over steep terrain.
Moist-layer depth
2631 m contiguous at or above 80% RH, 3163–5794 m across 700 hPa, 600 hPa, 500 hPa (lowest 80%). The layer runs into the top of the supplied profile, so its real depth is at least this and unknown above it. Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5373 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5783 m (4654 m).
Lowest-layer lapse rate
2.8 °C/km between the model surface (1129 m) and 850 hPa (1559 m) — stable — shallow fall with height. Measured across 430 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
No two adjacent supplied levels are both at or above 80% RH, so no depth can be measured. A single humid level is not a depth.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5370 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5787 m (4658 m).
Lowest-layer lapse rate
10.9 °C/km between the model surface (1129 m) and 850 hPa (1561 m) — at or above the dry adiabatic rate. Measured across 432 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
1223 m contiguous at or above 80% RH, 3157–4380 m across 700 hPa, 600 hPa (lowest 83%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5387 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5778 m (4649 m).
Lowest-layer lapse rate
8.1 °C/km between the model surface (1129 m) and 850 hPa (1550 m) — steep. Measured across 421 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
2630 m contiguous at or above 80% RH, 3148–5778 m across 700 hPa, 600 hPa, 500 hPa (lowest 80%). The layer runs into the top of the supplied profile, so its real depth is at least this and unknown above it. Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5405 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5779 m (4650 m).
Lowest-layer lapse rate
0.7 °C/km between the model surface (1129 m) and 850 hPa (1555 m) — stable — shallow fall with height. Measured across 426 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
2630 m contiguous at or above 80% RH, 3149–5779 m across 700 hPa, 600 hPa, 500 hPa (lowest 87%). The layer runs into the top of the supplied profile, so its real depth is at least this and unknown above it. Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5406 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5763 m (4634 m).
Lowest-layer lapse rate
3.3 °C/km between the model surface (1129 m) and 850 hPa (1547 m) — stable — shallow fall with height. Measured across 418 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
4634 m contiguous at or above 80% RH, 1129–5763 m across the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa (lowest 88%). The layer runs into the top of the supplied profile, so its real depth is at least this and unknown above it. Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5390 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5764 m (4635 m).
Lowest-layer lapse rate
7.3 °C/km between the model surface (1129 m) and 850 hPa (1554 m) — steep. Measured across 425 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
3231 m contiguous at or above 80% RH, 1129–4360 m across the model surface, 850 hPa, 700 hPa, 600 hPa (lowest 90%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5291 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5754 m (4625 m).
Lowest-layer lapse rate
7.1 °C/km between the model surface (1129 m) and 850 hPa (1549 m) — steep. Measured across 420 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
3224 m contiguous at or above 80% RH, 1129–4353 m across the model surface, 850 hPa, 700 hPa, 600 hPa (lowest 81%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5194 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5745 m (4616 m).
Lowest-layer lapse rate
4.8 °C/km between the model surface (1129 m) and 850 hPa (1549 m) — moderate — near the saturated rate. Measured across 420 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
2002 m contiguous at or above 80% RH, 1129–3131 m across the model surface, 850 hPa, 700 hPa (lowest 86%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5047 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 700 hPa, 600 hPa, 500 hPa — 5 levels spanning 1129–5721 m (4592 m).
Lowest-layer lapse rate
6.2 °C/km between the model surface (1129 m) and 850 hPa (1531 m) — moderate — near the saturated rate. Measured across 402 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
1982 m contiguous at or above 80% RH, 1129–3111 m across the model surface, 850 hPa, 700 hPa (lowest 82%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 4971 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1327–5790 m (4463 m).
Lowest-layer lapse rate
22.4 °C/km between the model surface (1327 m) and 850 hPa (1573 m) — at or above the dry adiabatic rate. Measured across 246 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
No two adjacent supplied levels are both at or above 80% RH, so no depth can be measured. A single humid level is not a depth.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5409 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1327–5782 m (4455 m).
Lowest-layer lapse rate
-9.9 °C/km between the model surface (1327 m) and 850 hPa (1559 m) — temperature rises with height. Measured across 232 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
  • 1327–1559 m (the model surface to 850 hPa): 10.4 °C rising to 12.7 °C, 9.9 °C/km of warming over 232 m.
A feature of this coarse model profile, not an observed inversion. It may equally be an artefact of interpolating a wide grid over steep terrain.
Moist-layer depth
No two adjacent supplied levels are both at or above 80% RH, so no depth can be measured. A single humid level is not a depth.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5483 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1327–5779 m (4452 m).
Lowest-layer lapse rate
-3.8 °C/km between the model surface (1327 m) and 850 hPa (1566 m) — temperature rises with height. Measured across 239 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
  • 1327–1566 m (the model surface to 850 hPa): 10.0 °C rising to 10.9 °C, 3.8 °C/km of warming over 239 m.
A feature of this coarse model profile, not an observed inversion. It may equally be an artefact of interpolating a wide grid over steep terrain.
Moist-layer depth
3710 m contiguous at or above 80% RH, 2069–5779 m across 800 hPa, 700 hPa, 600 hPa, 500 hPa (lowest 89%). The layer runs into the top of the supplied profile, so its real depth is at least this and unknown above it. Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5268 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1327–5768 m (4441 m).
Lowest-layer lapse rate
-9.3 °C/km between the model surface (1327 m) and 850 hPa (1554 m) — temperature rises with height. Measured across 227 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
  • 1327–1554 m (the model surface to 850 hPa): 9.0 °C rising to 11.1 °C, 9.3 °C/km of warming over 227 m.
A feature of this coarse model profile, not an observed inversion. It may equally be an artefact of interpolating a wide grid over steep terrain.
Moist-layer depth
2624 m contiguous at or above 80% RH, 3144–5768 m across 700 hPa, 600 hPa, 500 hPa (lowest 86%). The layer runs into the top of the supplied profile, so its real depth is at least this and unknown above it. Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5288 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1327–5765 m (4438 m).
Lowest-layer lapse rate
0 °C/km between the model surface (1327 m) and 850 hPa (1548 m) — near-isothermal. Measured across 221 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
2623 m contiguous at or above 80% RH, 3142–5765 m across 700 hPa, 600 hPa, 500 hPa (lowest 81%). The layer runs into the top of the supplied profile, so its real depth is at least this and unknown above it. Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5297 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1327–5762 m (4435 m).
Lowest-layer lapse rate
-20.3 °C/km between the model surface (1327 m) and 850 hPa (1524 m) — temperature rises with height. Measured across 197 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
  • 1327–1524 m (the model surface to 850 hPa): 10.1 °C rising to 14.1 °C, 20.3 °C/km of warming over 197 m.
A feature of this coarse model profile, not an observed inversion. It may equally be an artefact of interpolating a wide grid over steep terrain.
Moist-layer depth
1225 m contiguous at or above 80% RH, 3132–4357 m across 700 hPa, 600 hPa (lowest 90%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5328 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1327–5757 m (4430 m).
Lowest-layer lapse rate
3.7 °C/km between the model surface (1327 m) and 850 hPa (1543 m) — stable — shallow fall with height. Measured across 216 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
4430 m contiguous at or above 80% RH, 1327–5757 m across the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa (lowest 97%). The layer runs into the top of the supplied profile, so its real depth is at least this and unknown above it. Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5329 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1327–5741 m (4414 m).
Lowest-layer lapse rate
5.4 °C/km between the model surface (1327 m) and 850 hPa (1530 m) — moderate — near the saturated rate. Measured across 203 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
3010 m contiguous at or above 80% RH, 1327–4337 m across the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa (lowest 91%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5313 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1327–5718 m (4391 m).
Lowest-layer lapse rate
6 °C/km between the model surface (1327 m) and 850 hPa (1527 m) — moderate — near the saturated rate. Measured across 200 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
4391 m contiguous at or above 80% RH, 1327–5718 m across the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa (lowest 96%). The layer runs into the top of the supplied profile, so its real depth is at least this and unknown above it. Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5132 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1327–5711 m (4384 m).
Lowest-layer lapse rate
5.9 °C/km between the model surface (1327 m) and 850 hPa (1531 m) — moderate — near the saturated rate. Measured across 204 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
  • 1531–2025 m (850 hPa to 800 hPa): 4.6 °C rising to 5.1 °C, 1 °C/km of warming over 494 m.
A feature of this coarse model profile, not an observed inversion. It may equally be an artefact of interpolating a wide grid over steep terrain.
Moist-layer depth
204 m contiguous at or above 80% RH, 1327–1531 m across the model surface, 850 hPa (lowest 82%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5080 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1327–5696 m (4369 m).
Lowest-layer lapse rate
-1 °C/km between the model surface (1327 m) and 850 hPa (1537 m) — temperature rises with height. Measured across 210 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
  • 1327–1537 m (the model surface to 850 hPa): 5.4 °C rising to 5.6 °C, 1 °C/km of warming over 210 m.
A feature of this coarse model profile, not an observed inversion. It may equally be an artefact of interpolating a wide grid over steep terrain.
Moist-layer depth
1775 m contiguous at or above 80% RH, 1327–3102 m across the model surface, 850 hPa, 800 hPa, 700 hPa (lowest 87%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Covered by the supplied levels The supplied levels bracket both bounds: -12 °C at 4710 m and -18 °C at 5634 m, interpolated between adjacent supplied levels. Overlap is a property of this profile’s temperature structure — it is not a statement that snow is growing there.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1327–5676 m (4349 m).
Lowest-layer lapse rate
-3.8 °C/km between the model surface (1327 m) and 850 hPa (1535 m) — temperature rises with height. Measured across 208 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
  • 1327–1535 m (the model surface to 850 hPa): 5.4 °C rising to 6.2 °C, 3.8 °C/km of warming over 208 m.
A feature of this coarse model profile, not an observed inversion. It may equally be an artefact of interpolating a wide grid over steep terrain.
Moist-layer depth
2971 m contiguous at or above 80% RH, 1327–4298 m across the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa (lowest 86%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Covered by the supplied levels The supplied levels bracket both bounds: -12 °C at 4393 m and -18 °C at 5343 m, interpolated between adjacent supplied levels. Overlap is a property of this profile’s temperature structure — it is not a statement that snow is growing there.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1352–5799 m (4447 m).
Lowest-layer lapse rate
15.4 °C/km between the model surface (1352 m) and 850 hPa (1573 m) — at or above the dry adiabatic rate. Measured across 221 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
No two adjacent supplied levels are both at or above 80% RH, so no depth can be measured. A single humid level is not a depth.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5571 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1352–5787 m (4435 m).
Lowest-layer lapse rate
0.5 °C/km between the model surface (1352 m) and 850 hPa (1565 m) — near-isothermal. Measured across 213 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
No two adjacent supplied levels are both at or above 80% RH, so no depth can be measured. A single humid level is not a depth.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5482 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1352–5786 m (4434 m).
Lowest-layer lapse rate
-1.4 °C/km between the model surface (1352 m) and 850 hPa (1561 m) — temperature rises with height. Measured across 209 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
  • 1352–1561 m (the model surface to 850 hPa): 12.3 °C rising to 12.6 °C, 1.4 °C/km of warming over 209 m.
A feature of this coarse model profile, not an observed inversion. It may equally be an artefact of interpolating a wide grid over steep terrain.
Moist-layer depth
2312 m contiguous at or above 80% RH, 2066–4378 m across 800 hPa, 700 hPa, 600 hPa (lowest 81%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5351 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1352–5775 m (4423 m).
Lowest-layer lapse rate
-1 °C/km between the model surface (1352 m) and 850 hPa (1553 m) — temperature rises with height. Measured across 201 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
  • 1352–1553 m (the model surface to 850 hPa): 10.7 °C rising to 10.9 °C, 1 °C/km of warming over 201 m.
A feature of this coarse model profile, not an observed inversion. It may equally be an artefact of interpolating a wide grid over steep terrain.
Moist-layer depth
2312 m contiguous at or above 80% RH, 2056–4368 m across 800 hPa, 700 hPa, 600 hPa (lowest 83%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5482 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1352–5771 m (4419 m).
Lowest-layer lapse rate
13.4 °C/km between the model surface (1352 m) and 850 hPa (1553 m) — at or above the dry adiabatic rate. Measured across 201 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
2308 m contiguous at or above 80% RH, 2052–4360 m across 800 hPa, 700 hPa, 600 hPa (lowest 85%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5536 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1352–5766 m (4414 m).
Lowest-layer lapse rate
3 °C/km between the model surface (1352 m) and 850 hPa (1553 m) — stable — shallow fall with height. Measured across 201 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
3009 m contiguous at or above 80% RH, 1352–4361 m across the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa (lowest 87%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5375 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1352–5768 m (4416 m).
Lowest-layer lapse rate
-0.5 °C/km between the model surface (1352 m) and 850 hPa (1553 m) — near-isothermal. Measured across 201 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
  • 1352–1553 m (the model surface to 850 hPa): 9.6 °C rising to 9.7 °C, 0.5 °C/km of warming over 201 m.
A feature of this coarse model profile, not an observed inversion. It may equally be an artefact of interpolating a wide grid over steep terrain.
Moist-layer depth
4416 m contiguous at or above 80% RH, 1352–5768 m across the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa (lowest 92%). The layer runs into the top of the supplied profile, so its real depth is at least this and unknown above it. Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5277 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1352–5754 m (4402 m).
Lowest-layer lapse rate
2.6 °C/km between the model surface (1352 m) and 850 hPa (1547 m) — stable — shallow fall with height. Measured across 195 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
4402 m contiguous at or above 80% RH, 1352–5754 m across the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa (lowest 91%). The layer runs into the top of the supplied profile, so its real depth is at least this and unknown above it. Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5244 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1352–5735 m (4383 m).
Lowest-layer lapse rate
5.1 °C/km between the model surface (1352 m) and 850 hPa (1547 m) — moderate — near the saturated rate. Measured across 195 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
2989 m contiguous at or above 80% RH, 1352–4341 m across the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa (lowest 94%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Partially covered The -12 °C bound is at 5078 m; the -18 °C bound lies above 500 hPa, the highest level supplied, and is not extrapolated to. The depth of the overlap is therefore a lower bound, not a measurement.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1352–5727 m (4375 m).
Lowest-layer lapse rate
1.5 °C/km between the model surface (1352 m) and 850 hPa (1552 m) — stable — shallow fall with height. Measured across 200 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
  • 1552–2048 m (850 hPa to 800 hPa): 5.1 °C rising to 5.4 °C, 0.6 °C/km of warming over 496 m.
A feature of this coarse model profile, not an observed inversion. It may equally be an artefact of interpolating a wide grid over steep terrain.
Moist-layer depth
1776 m contiguous at or above 80% RH, 1352–3128 m across the model surface, 850 hPa, 800 hPa, 700 hPa (lowest 91%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Covered by the supplied levels The supplied levels bracket both bounds: -12 °C at 4830 m and -18 °C at 5671 m, interpolated between adjacent supplied levels. Overlap is a property of this profile’s temperature structure — it is not a statement that snow is growing there.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1352–5712 m (4360 m).
Lowest-layer lapse rate
-1.5 °C/km between the model surface (1352 m) and 850 hPa (1548 m) — temperature rises with height. Measured across 196 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
  • 1352–1548 m (the model surface to 850 hPa): 5.4 °C rising to 5.7 °C, 1.5 °C/km of warming over 196 m.
A feature of this coarse model profile, not an observed inversion. It may equally be an artefact of interpolating a wide grid over steep terrain.
Moist-layer depth
693 m contiguous at or above 80% RH, 1352–2045 m across the model surface, 850 hPa, 800 hPa (lowest 94%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Covered by the supplied levels The supplied levels bracket both bounds: -12 °C at 4689 m and -18 °C at 5518 m, interpolated between adjacent supplied levels. Overlap is a property of this profile’s temperature structure — it is not a statement that snow is growing there.

Complete supplied-profile diagnostics

Uses every genuine supplied level through the profile top, regardless of the selected chart view.

Supplied levels
the model surface, 850 hPa, 800 hPa, 700 hPa, 600 hPa, 500 hPa — 6 levels spanning 1352–5678 m (4326 m).
Lowest-layer lapse rate
0.6 °C/km between the model surface (1352 m) and 850 hPa (1529 m) — stable — shallow fall with height. Measured across 177 m, so it is a layer average and cannot resolve structure inside that depth.
Modelled inversions
None between adjacent supplied levels. That is not the same as no inversion: one shallower than the gap between two levels would not appear here at all.
Moist-layer depth
1744 m contiguous at or above 80% RH, 1352–3096 m across the model surface, 850 hPa, 800 hPa, 700 hPa (lowest 97%). Descriptive moisture depth — where the model is humid. Not proof of cloud, and not proof of snowfall.
Dendritic growth range (-12 to -18 °C)
Covered by the supplied levels The supplied levels bracket both bounds: -12 °C at 4578 m and -18 °C at 5373 m, interpolated between adjacent supplied levels. Overlap is a property of this profile’s temperature structure — it is not a statement that snow is growing there.
What this page does not claim
  • This is a model profile, not a sounding. There is no radiosonde in it. The nearest upper-air site to the Australian Alps is hundreds of kilometres away, and no observed sounding is drawn on this chart — nor is the surface observation from /now, which is one instrument at one height and would be a fabrication if plotted as a column.
  • Coverage is sparse and model-dependent. Below-terrain levels are already excluded, which at an alpine grid point routinely removes 1000 and 925 hPa. An ECMWF profile includes 850, 700, 600 and 500 hPa above the surface when all requested triplets are present.
  • Nothing is extrapolated above the requested 500 hPa level. Where the dendritic range sits above the supplied profile top, the page says the supplied levels do not cover it — never that there is no dendritic zone.
  • No amount, no score. Deeper moisture and a bracketed dendritic range are structural facts about the profile. Turning them into centimetres or a “powder rating” would be inventing a number the data cannot support.
  • ACCESS-G has no point profile here. Its Open-Meteo domain has not initialised since June 2025 and returns an all-null series; an empty profile with a model’s name on it is worse than no chart. The Bureau’s current ACCESS-G chart products are available in the app’s live ACCESS-G map viewer.