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| NWRFC Model Parameters | NWRFC Model Simulations | NOHRSC | |||||||||||
ID | Elev Range (feet) | SI (inches) | AccMax (inches) | Date | SWE (inches) | Pct Avg | SWE Avg 1991-2020 (inches) | SWE Max 1991-2020 (inches) | SWE Min 1991-2020 (inches) | Snow Cover Extent | Snow Line (feet) | SWE (inches) | Snow Cover Extent |
| PACW4L | 6752-8500 | 23.62 | ----- | 06-01 | 0.32 | 13 % | 2.5 | 15.8 | 0.0 | 0.07 | 8389 | 0.1 | 0.37 |
| PACW4U | 8500-10224 | 393.66 | ----- | 06-01 | 5.95 | 52 % | 11.4 | 38.9 | 0.0 | 1.00 | 8500 | 4.7 | 0.88 |
| Simulated Basin Average | 45 % | ||||||||||||
ID | Name | Distance (miles) | Elevation (feet) | Date | SWE | Pct Avg | SWE Avg 1991-2020 | Snow Depth (inches) | Snow Density | Pct Curr Peak | Pct Avg Peak |
| SNKE R ON JACKSN LK AT DM TB20 | 0 | 6728 | 06-01 | N/A | N/A | N/A | N/A | N/A | N/A | ||
| SNAKE RIVER STATION SNOTEL | 12 | 6920 | 06-01 | 0.0 | 0 % | 0.1 | 0 | -- % | 0 % | 0 % | |
| BASECAMP SNOTEL | 0 | 7030 | 06-01 | 0.0 | 0 % | 0.4 | 0 | -- % | 0 % | 0 % | |
| GLADE CREEK NR MORAN | 16 | 7040 | 06-01 | N/A | N/A | N/A | N/A | N/A | N/A | ||
| GRASSY LAKE SNOTEL | 20 | 7265 | 06-01 | 0.0 | 0 % | 7.9 | 0 | -- % | 0 % | 0 % | |
| HUCKLEBERRY DIV NR MORAN TB30 | 12 | 7300 | 06-01 | N/A | N/A | N/A | N/A | N/A | N/A | ||
| LEWIS LAKE DIVIDE SNOTEL | 15 | 7860 | 06-01 | 0.0 | 0 % | 12.0 | 0 | -- % | 0 % | 0 % | |
| YOUNTS PEAK SNOTEL | 16 | 8350 | 06-02 | 0.0 | N/A | 0 | -- % | 0 % | -- | ||
| GRAND TARGHEE | 18 | 9260 | 06-01 | 21.3 | 54 % | 39.7 | 48 | 44 % | 57 % | 44 % | |
| TWO OCEAN PLATEAU SNOTEL | 2 | 9360 | 06-02 | 23.0 | 95 % | 24.3 | 35 | 66 % | 64 % | 68 % | |
| TOGWOTEE PASS SNOTEL | 16 | 9580 | 06-02 | 6.8 | 37 % | 18.2 | 14 | 49 % | 31 % | 26 % | |
| Observed Basin Average | 50 % | ||||||||||
| Please Note: Snow stations highlighted in cyan have no historic normals from the reporting agency and are not included in the basin average calculation. | |||||||||||
| Please Note: Snow stations highlighted in red have no current swe observation and are not included in the basin average caclulation. | |||||||||||
