Snow level against each resort’s terrain, with precipitation phase at the selected lifted elevation.
Every resort is deselected, so there is nothing to show. Choose at least one above.
Applies to the snow-level charts and precipitation phase below.
ACCESS-G is running, but its free point-data relay is not. Current Bureau rainfall, pressure, 850 hPa temperature and humidity remain available in the ACCESS-G map viewer.
| Resort | ECMWF IFS | ECMWF AIFS | GFS | ICON | ACCESS-G | UKMO Global | JMA GSM |
|---|---|---|---|---|---|---|---|
| Perisher 1824 m | 1.4 / 8.6 | 0.6 / 2.8 | 15.2 / 15.3 | 13 / 13 | — | 21.7 / 29 | 0.6 / 0.6 |
| Thredbo 1701 m | 14.7 / 25.4 | 5.4 / 13.1 | 11 / 11 | 4.8 / 9.7 | — | 5 / 17.6 | 0.5 / 0.6 |
| Charlotte Pass 1860 m | 21.9 / 25.4 | 6.2 / 13.1 | 15.2 / 15.3 | 13 / 13 | — | 12.3 / 17.6 | 0.5 / 0.6 |
| Selwyn 1553 m | 4.5 / 10.6 | 3 / 10.6 | 9.6 / 10.7 | 2.9 / 10.3 | — | 6.2 / 17.1 | 5.6 / 9.3 |
| Mt Hotham 1648 m | 7.6 / 17.6 | 5.3 / 13.2 | 23.8 / 25.4 | 1.2 / 13 | — | 20.3 / 55.1 | 13 / 19.6 |
| Falls Creek 1640 m | 13.9 / 30.3 | 7.5 / 20.5 | 23.3 / 25 | 4.5 / 20.7 | — | 13.6 / 45.9 | 1.2 / 2.8 |
| Mt Buller 1578 m | 12.9 / 25.9 | 6.9 / 18.3 | 27.1 / 29.5 | 6.7 / 28.4 | — | 13.6 / 50.2 | 9.6 / 22.9 |
| Mt Baw Baw 1507 m | 6.3 / 30.1 | 1.8 / 17.9 | 9 / 31.6 | 1.8 / 10.5 | — | 3.1 / 47.3 | 3.1 / 11 |
Daily values are AEST, in mm liquid equivalent. The final column is each forecast’s full-window sum. Forecast rows follow the selected primary/comparison models. The local 9 km reference follows the ECMWF IFS selection, with unphased precipitation and native SWE shown separately. For a longer selectable period, open the model explorer.
| Resort | Forecast | Sun 2 | Mon 3 | Tue 4 | Wed 5 | Thu 6 | Fri 7 | Sat 8 | Sun 9 | Total |
|---|---|---|---|---|---|---|---|---|---|---|
| Perisher | ECMWF IFS | 0 | 1.2 | 0.6 | 0 | 0 | 0 | 0.3 | 6.5 | 8.6 |
| Perisher | ECMWF AIFS | 0 | 0 | 0 | 0.6 | 0 | 0 | 0.2 | 2 | 2.8 |
| Perisher | GFS | 0 | 0 | 6.7 | 6.7 | 0 | 0.1 | 0 | 1.8 | 15.3 |
| Perisher | ICON | 0 | 0 | 3.6 | 3.3 | 0 | 0 | 0 | 6.1 | 13 |
| Perisher | UKMO Global | 0.2 | 5 | 6.7 | 4.1 | 0 | 0 | 2 | 11 | 29 |
| Perisher | JMA GSM | 0 | 0 | 0 | 0 | 0 | 0 | 0.6 | 0 | 0.6 |
| Perisher | IFS 9 km surface · unphased precip | 0 | 0.5 | 4.1 | 3.5 | 0 | 0 | 0.6 | 11.5 | 20.2 |
| Perisher | IFS 9 km surface · native SWE | 0 | 0.1 | 3.7 | 1.5 | 0 | 0 | 0.6 | 10 | 15.9 |
| Thredbo | ECMWF IFS | 0 | 1.8 | 4.6 | 3.8 | 0 | 0 | 0.7 | 14.5 | 25.4 |
| Thredbo | ECMWF AIFS | 0.1 | 1.8 | 2.4 | 2.9 | 0 | 0 | 0.4 | 5.5 | 13.1 |
| Thredbo | GFS | 0 | 0 | 5.2 | 4.8 | 0 | 0 | 0 | 1 | 11 |
| Thredbo | ICON | 0 | 0.2 | 1.9 | 1.5 | 0 | 0 | 0 | 6.1 | 9.7 |
| Thredbo | UKMO Global | 0.4 | 3.2 | 2.1 | 1.1 | 0 | 0 | 1.8 | 9 | 17.6 |
| Thredbo | JMA GSM | 0 | 0 | 0 | 0 | 0 | 0 | 0.6 | 0 | 0.6 |
| Thredbo | IFS 9 km surface · unphased precip | 0 | 0.7 | 1.6 | 0.8 | 0 | 0 | 0.5 | 11 | 14.6 |
| Thredbo | IFS 9 km surface · native SWE | 0 | 0.3 | 1.8 | 0.4 | 0 | 0 | 0.5 | 10 | 13 |
| Charlotte Pass | ECMWF IFS | 0 | 1.8 | 4.6 | 3.8 | 0 | 0 | 0.7 | 14.5 | 25.4 |
| Charlotte Pass | ECMWF AIFS | 0.1 | 1.8 | 2.4 | 2.9 | 0 | 0 | 0.4 | 5.5 | 13.1 |
| Charlotte Pass | GFS | 0 | 0 | 6.7 | 6.7 | 0 | 0.1 | 0 | 1.8 | 15.3 |
| Charlotte Pass | ICON | 0 | 0 | 3.6 | 3.3 | 0 | 0 | 0 | 6.1 | 13 |
| Charlotte Pass | UKMO Global | 0.4 | 3.2 | 2.1 | 1.1 | 0 | 0 | 1.8 | 9 | 17.6 |
| Charlotte Pass | JMA GSM | 0 | 0 | 0 | 0 | 0 | 0 | 0.6 | 0 | 0.6 |
| Charlotte Pass | IFS 9 km surface · unphased precip | 0 | 1.3 | 9.8 | 10.1 | 0 | 0 | 0.9 | 15.5 | 37.6 |
| Charlotte Pass | IFS 9 km surface · native SWE | 0 | 0.6 | 8.6 | 5.2 | 0 | 0 | 0.9 | 13 | 28.3 |
| Selwyn | ECMWF IFS | 0 | 0.3 | 1 | 3.5 | 0 | 0 | 0.3 | 5.5 | 10.6 |
| Selwyn | ECMWF AIFS | 0.1 | 1.1 | 1.3 | 1.7 | 0 | 0 | 0.4 | 6 | 10.6 |
| Selwyn | GFS | 0.2 | 0 | 5.2 | 3.5 | 0 | 0 | 0 | 1.8 | 10.7 |
| Selwyn | ICON | 0 | 0 | 3 | 0.2 | 0 | 0 | 0 | 7.1 | 10.3 |
| Selwyn | UKMO Global | 0 | 1.1 | 2.9 | 3.1 | 0.5 | 0 | 1 | 8.5 | 17.1 |
| Selwyn | JMA GSM | 0 | 0.5 | 4.4 | 1.2 | 0.5 | 0 | 0.2 | 2.5 | 9.3 |
| Selwyn | IFS 9 km surface · unphased precip | 0 | 0.7 | 2.4 | 3.9 | 0 | 0 | 0.4 | 9 | 16.4 |
| Selwyn | IFS 9 km surface · native SWE | 0 | 0 | 1.9 | 1.3 | 0 | 0 | 0.4 | 6 | 9.6 |
| Mt Hotham | ECMWF IFS | 0 | 0.7 | 2.1 | 0.5 | 0 | 0 | 0.8 | 13.5 | 17.6 |
| Mt Hotham | ECMWF AIFS | 0.2 | 1.8 | 2.9 | 2.3 | 0 | 0 | 0.5 | 5.5 | 13.2 |
| Mt Hotham | GFS | 0.5 | 2.7 | 7.9 | 8 | 0 | 0 | 0 | 6.3 | 25.4 |
| Mt Hotham | ICON | 0 | 0.1 | 0.8 | 0.3 | 0 | 0.3 | 0.3 | 11.2 | 13 |
| Mt Hotham | UKMO Global | 1.2 | 6.2 | 10.1 | 6.6 | 0 | 0 | 8 | 23 | 55.1 |
| Mt Hotham | JMA GSM | 0 | 3.4 | 8.1 | 1.1 | 0 | 0.1 | 0.8 | 5.5 | 19 |
| Mt Hotham | IFS 9 km surface · unphased precip | 0 | 1.3 | 5.6 | 5.8 | 0 | 0 | 1.9 | 19 | 33.6 |
| Mt Hotham | IFS 9 km surface · native SWE | 0 | 0.7 | 3.8 | 1.7 | 0 | 0 | 1.8 | 15.5 | 23.5 |
| Falls Creek | ECMWF IFS | 0.1 | 1.9 | 4.7 | 3.3 | 0.5 | 0 | 2.3 | 17.5 | 30.3 |
| Falls Creek | ECMWF AIFS | 0.2 | 3 | 3.6 | 2.8 | 0 | 0 | 1.4 | 9.5 | 20.5 |
| Falls Creek | GFS | 0.6 | 1.3 | 8.5 | 7.2 | 0 | 0 | 0 | 7.4 | 25 |
| Falls Creek | ICON | 0 | 0 | 1.4 | 0.8 | 0 | 0 | 0.3 | 18.2 | 20.7 |
| Falls Creek | UKMO Global | 1.1 | 5.6 | 7.2 | 3.1 | 0 | 0 | 7.4 | 21.5 | 45.9 |
| Falls Creek | JMA GSM | 0 | 0.2 | 1 | 0 | 0 | 0 | -0.5 | 1.5 | 2.2 |
| Falls Creek | IFS 9 km surface · unphased precip | 0 | 0 | 2.7 | 3.5 | 0 | 0 | 1.5 | 18 | 25.7 |
| Falls Creek | IFS 9 km surface · native SWE | 0 | 0 | 2.4 | 1.3 | 0 | 0 | 1.5 | 17.5 | 22.7 |
| Mt Buller | ECMWF IFS | 0.1 | 3.4 | 5.6 | 2.1 | 0.2 | 0 | 2.5 | 12 | 25.9 |
| Mt Buller | ECMWF AIFS | 0.1 | 1.9 | 4.7 | 2.3 | 0 | 0 | 1.3 | 8 | 18.3 |
| Mt Buller | GFS | 0.1 | 4.5 | 13.5 | 3.5 | 0 | 0 | 0 | 7.9 | 29.5 |
| Mt Buller | ICON | 0 | 2.3 | 4.9 | 1 | 0 | 0 | 1.4 | 18.8 | 28.4 |
| Mt Buller | UKMO Global | 0.2 | 4.7 | 15.5 | 7.1 | 0 | 0 | 8.7 | 14 | 50.2 |
| Mt Buller | JMA GSM | 0 | 4.2 | 6.1 | 1.1 | 0 | 0 | 2 | 9.5 | 22.9 |
| Mt Buller | IFS 9 km surface · unphased precip | 0 | 4.1 | 7.8 | 5.6 | 0.6 | 0 | 2.8 | 14 | 34.9 |
| Mt Buller | IFS 9 km surface · native SWE | 0 | 0 | 1.2 | 0.4 | 0 | 0 | 0.1 | 3.5 | 5.2 |
| Mt Baw Baw | ECMWF IFS | 0 | 2.8 | 7.5 | 8.7 | 2 | 0 | 1.6 | 7.5 | 30.1 |
| Mt Baw Baw | ECMWF AIFS | 0 | 1.3 | 5.5 | 5.2 | 0 | 0 | 0.9 | 5 | 17.9 |
| Mt Baw Baw | GFS | 0 | 1.1 | 11.1 | 16.6 | 0.7 | 0.1 | 0 | 2 | 31.6 |
| Mt Baw Baw | ICON | 0 | 1.1 | 3.6 | 0.8 | 0 | 0 | 0.2 | 4.8 | 10.5 |
| Mt Baw Baw | UKMO Global | 0 | 2.3 | 17.8 | 22.2 | 0.7 | 0 | 0.8 | 3.5 | 47.3 |
| Mt Baw Baw | JMA GSM | 0 | 0.8 | 4.7 | 2.9 | 0 | 0 | 0.6 | 2 | 11 |
| Mt Baw Baw | IFS 9 km surface · unphased precip | 0 | 0.9 | 6.1 | 9.4 | 1 | 0 | 0.9 | 6.5 | 24.8 |
| Mt Baw Baw | IFS 9 km surface · native SWE | 0 | 0 | 0.5 | 0 | 0 | 0 | 0 | 0.5 | 1 |
Where the wet-bulb is already below zero at a model’s grid terrain, the continuous line extends downward using a 6.5 °C/km environmental lapse-rate estimate, with the uncertainty band widened across a 4.5–8.5 °C/km range. It is useful below-terrain guidance, not a model level directly resolved there.
Dashed sections stop at the model’s grid terrain. They are upper bounds: the wet-bulb zero is somewhere at or below that height, but this view does not estimate how far below. Phase below the bound remains uncertain.
The shaded band is a heuristic uncertainty around ECMWF IFS’s snow level. Each coloured snow-level line is emphasised where that model forecasts precipitation. The selected precipitation model receives the strongest emphasis because it also supplies the primary histogram and headline; other wet model lines remain medium-weight. Phase colours and totals here are judged at Mid · 1824 m.
Model-grid SWE is ECMWF IFS’s native sf field (parameter 144),
expressed as liquid water equivalent at the model grid cell and its terrain. It is
shown as an independent comparison: it does not alter the resort-elevation wet-bulb
phase analysis and is not a settled-snow depth.
IFS 9 km surface is a separate native-resolution deterministic IFS surface sample. Its precipitation bars are intentionally unphased: this feed does not supply the pressure-level temperature/humidity profile used by the snow-level method. Native SWE is shown independently and does not alter the 25 km profile or ensemble products. Sampled cell -36.380, 148.435 · model terrain 1621 m · Sun 2 1600hrs AEST · 0600Z.
Model comparison, run times and meteograms for Perisher → · ACCESS-G currently unavailable
Where the wet-bulb is already below zero at a model’s grid terrain, the continuous line extends downward using a 6.5 °C/km environmental lapse-rate estimate, with the uncertainty band widened across a 4.5–8.5 °C/km range. It is useful below-terrain guidance, not a model level directly resolved there.
Dashed sections stop at the model’s grid terrain. They are upper bounds: the wet-bulb zero is somewhere at or below that height, but this view does not estimate how far below. Phase below the bound remains uncertain.
The shaded band is a heuristic uncertainty around ECMWF IFS’s snow level. Each coloured snow-level line is emphasised where that model forecasts precipitation. The selected precipitation model receives the strongest emphasis because it also supplies the primary histogram and headline; other wet model lines remain medium-weight. Phase colours and totals here are judged at Mid · 1701 m.
Model-grid SWE is ECMWF IFS’s native sf field (parameter 144),
expressed as liquid water equivalent at the model grid cell and its terrain. It is
shown as an independent comparison: it does not alter the resort-elevation wet-bulb
phase analysis and is not a settled-snow depth.
IFS 9 km surface is a separate native-resolution deterministic IFS surface sample. Its precipitation bars are intentionally unphased: this feed does not supply the pressure-level temperature/humidity profile used by the snow-level method. Native SWE is shown independently and does not alter the 25 km profile or ensemble products. Sampled cell -36.520, 148.353 · model terrain 1644 m · Sun 2 1600hrs AEST · 0600Z.
Model comparison, run times and meteograms for Thredbo → · ACCESS-G currently unavailable
Where the wet-bulb is already below zero at a model’s grid terrain, the continuous line extends downward using a 6.5 °C/km environmental lapse-rate estimate, with the uncertainty band widened across a 4.5–8.5 °C/km range. It is useful below-terrain guidance, not a model level directly resolved there.
Dashed sections stop at the model’s grid terrain. They are upper bounds: the wet-bulb zero is somewhere at or below that height, but this view does not estimate how far below. Phase below the bound remains uncertain.
The shaded band is a heuristic uncertainty around ECMWF IFS’s snow level. Each coloured snow-level line is emphasised where that model forecasts precipitation. The selected precipitation model receives the strongest emphasis because it also supplies the primary histogram and headline; other wet model lines remain medium-weight. Phase colours and totals here are judged at Mid · 1860 m.
Model-grid SWE is ECMWF IFS’s native sf field (parameter 144),
expressed as liquid water equivalent at the model grid cell and its terrain. It is
shown as an independent comparison: it does not alter the resort-elevation wet-bulb
phase analysis and is not a settled-snow depth.
IFS 9 km surface is a separate native-resolution deterministic IFS surface sample. Its precipitation bars are intentionally unphased: this feed does not supply the pressure-level temperature/humidity profile used by the snow-level method. Native SWE is shown independently and does not alter the 25 km profile or ensemble products. Sampled cell -36.380, 148.318 · model terrain 1613 m · Sun 2 1600hrs AEST · 0600Z.
Model comparison, run times and meteograms for Charlotte Pass → · ACCESS-G currently unavailable
Where the wet-bulb is already below zero at a model’s grid terrain, the continuous line extends downward using a 6.5 °C/km environmental lapse-rate estimate, with the uncertainty band widened across a 4.5–8.5 °C/km range. It is useful below-terrain guidance, not a model level directly resolved there.
Dashed sections stop at the model’s grid terrain. They are upper bounds: the wet-bulb zero is somewhere at or below that height, but this view does not estimate how far below. Phase below the bound remains uncertain.
The shaded band is a heuristic uncertainty around ECMWF IFS’s snow level. Each coloured snow-level line is emphasised where that model forecasts precipitation. The selected precipitation model receives the strongest emphasis because it also supplies the primary histogram and headline; other wet model lines remain medium-weight. Phase colours and totals here are judged at Mid · 1553 m.
Model-grid SWE is ECMWF IFS’s native sf field (parameter 144),
expressed as liquid water equivalent at the model grid cell and its terrain. It is
shown as an independent comparison: it does not alter the resort-elevation wet-bulb
phase analysis and is not a settled-snow depth.
IFS 9 km surface is a separate native-resolution deterministic IFS surface sample. Its precipitation bars are intentionally unphased: this feed does not supply the pressure-level temperature/humidity profile used by the snow-level method. Native SWE is shown independently and does not alter the 25 km profile or ensemble products. Sampled cell -35.888, 148.488 · model terrain 1400 m · Sun 2 1600hrs AEST · 0600Z.
Model comparison, run times and meteograms for Selwyn → · ACCESS-G currently unavailable
Where the wet-bulb is already below zero at a model’s grid terrain, the continuous line extends downward using a 6.5 °C/km environmental lapse-rate estimate, with the uncertainty band widened across a 4.5–8.5 °C/km range. It is useful below-terrain guidance, not a model level directly resolved there.
Dashed sections stop at the model’s grid terrain. They are upper bounds: the wet-bulb zero is somewhere at or below that height, but this view does not estimate how far below. Phase below the bound remains uncertain.
The shaded band is a heuristic uncertainty around ECMWF IFS’s snow level. Each coloured snow-level line is emphasised where that model forecasts precipitation. The selected precipitation model receives the strongest emphasis because it also supplies the primary histogram and headline; other wet model lines remain medium-weight. Phase colours and totals here are judged at Mid · 1648 m.
Model-grid SWE is ECMWF IFS’s native sf field (parameter 144),
expressed as liquid water equivalent at the model grid cell and its terrain. It is
shown as an independent comparison: it does not alter the resort-elevation wet-bulb
phase analysis and is not a settled-snow depth.
IFS 9 km surface is a separate native-resolution deterministic IFS surface sample. Its precipitation bars are intentionally unphased: this feed does not supply the pressure-level temperature/humidity profile used by the snow-level method. Native SWE is shown independently and does not alter the 25 km profile or ensemble products. Sampled cell -36.942, 147.154 · model terrain 1388 m · Sun 2 1600hrs AEST · 0600Z.
Model comparison, run times and meteograms for Mt Hotham → · ACCESS-G currently unavailable
Where the wet-bulb is already below zero at a model’s grid terrain, the continuous line extends downward using a 6.5 °C/km environmental lapse-rate estimate, with the uncertainty band widened across a 4.5–8.5 °C/km range. It is useful below-terrain guidance, not a model level directly resolved there.
Dashed sections stop at the model’s grid terrain. They are upper bounds: the wet-bulb zero is somewhere at or below that height, but this view does not estimate how far below. Phase below the bound remains uncertain.
The shaded band is a heuristic uncertainty around ECMWF IFS’s snow level. Each coloured snow-level line is emphasised where that model forecasts precipitation. The selected precipitation model receives the strongest emphasis because it also supplies the primary histogram and headline; other wet model lines remain medium-weight. Phase colours and totals here are judged at Mid · 1640 m.
Model-grid SWE is ECMWF IFS’s native sf field (parameter 144),
expressed as liquid water equivalent at the model grid cell and its terrain. It is
shown as an independent comparison: it does not alter the resort-elevation wet-bulb
phase analysis and is not a settled-snow depth.
IFS 9 km surface is a separate native-resolution deterministic IFS surface sample. Its precipitation bars are intentionally unphased: this feed does not supply the pressure-level temperature/humidity profile used by the snow-level method. Native SWE is shown independently and does not alter the 25 km profile or ensemble products. Sampled cell -36.872, 147.316 · model terrain 1523 m · Sun 2 1600hrs AEST · 0600Z.
Model comparison, run times and meteograms for Falls Creek → · ACCESS-G currently unavailable
Where the wet-bulb is already below zero at a model’s grid terrain, the continuous line extends downward using a 6.5 °C/km environmental lapse-rate estimate, with the uncertainty band widened across a 4.5–8.5 °C/km range. It is useful below-terrain guidance, not a model level directly resolved there.
Dashed sections stop at the model’s grid terrain. They are upper bounds: the wet-bulb zero is somewhere at or below that height, but this view does not estimate how far below. Phase below the bound remains uncertain.
The shaded band is a heuristic uncertainty around ECMWF IFS’s snow level. Each coloured snow-level line is emphasised where that model forecasts precipitation. The selected precipitation model receives the strongest emphasis because it also supplies the primary histogram and headline; other wet model lines remain medium-weight. Phase colours and totals here are judged at Mid · 1578 m.
Model-grid SWE is ECMWF IFS’s native sf field (parameter 144),
expressed as liquid water equivalent at the model grid cell and its terrain. It is
shown as an independent comparison: it does not alter the resort-elevation wet-bulb
phase analysis and is not a settled-snow depth.
IFS 9 km surface is a separate native-resolution deterministic IFS surface sample. Its precipitation bars are intentionally unphased: this feed does not supply the pressure-level temperature/humidity profile used by the snow-level method. Native SWE is shown independently and does not alter the 25 km profile or ensemble products. Sampled cell -37.153, 146.429 · model terrain 1055 m · Sun 2 1600hrs AEST · 0600Z.
Model comparison, run times and meteograms for Mt Buller → · ACCESS-G currently unavailable
Where the wet-bulb is already below zero at a model’s grid terrain, the continuous line extends downward using a 6.5 °C/km environmental lapse-rate estimate, with the uncertainty band widened across a 4.5–8.5 °C/km range. It is useful below-terrain guidance, not a model level directly resolved there.
Dashed sections stop at the model’s grid terrain. They are upper bounds: the wet-bulb zero is somewhere at or below that height, but this view does not estimate how far below. Phase below the bound remains uncertain.
The shaded band is a heuristic uncertainty around ECMWF IFS’s snow level. Each coloured snow-level line is emphasised where that model forecasts precipitation. The selected precipitation model receives the strongest emphasis because it also supplies the primary histogram and headline; other wet model lines remain medium-weight. Phase colours and totals here are judged at Mid · 1507 m.
Model-grid SWE is ECMWF IFS’s native sf field (parameter 144),
expressed as liquid water equivalent at the model grid cell and its terrain. It is
shown as an independent comparison: it does not alter the resort-elevation wet-bulb
phase analysis and is not a settled-snow depth.
IFS 9 km surface is a separate native-resolution deterministic IFS surface sample. Its precipitation bars are intentionally unphased: this feed does not supply the pressure-level temperature/humidity profile used by the snow-level method. Native SWE is shown independently and does not alter the 25 km profile or ensemble products. Sampled cell -37.786, 146.265 · model terrain 936 m · Sun 2 1600hrs AEST · 0600Z.
Model comparison, run times and meteograms for Mt Baw Baw → · ACCESS-G currently unavailable