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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 |
| TRYO3L | 1586-4500 | 7.87 | ----- | 04-25 | 0.00 | N/A | 0.0 | 0.0 | 0.0 | 0.00 | --- | 0.2 | 0.03 |
| TRYO3U | 4500-9880 | 11.81 | ----- | 04-25 | 3.31 | 58 % | 5.7 | 14.1 | 0.0 | 0.24 | 6605 | 11.8 | 0.72 |
| Simulated Basin Average | 58 % | ||||||||||||
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 |
| BOWMAN SPRINGS SNOTEL | 0 | 4580 | 04-26 | 1.4 | 350 % | 0.4 | 0 | -- % | 15 % | 20 % | |
| COUNTY LINE SNOTEL | 0 | 4800 | 04-26 | 0.9 | N/A | 0.0 | 0 | -- % | 22 % | 26 % | |
| HIGH RIDGE SNOTEL | 1 | 4980 | 04-26 | 15.4 | 93 % | 16.6 | 34 | 45 % | 67 % | 68 % | |
| BEAVER RESERVOIR SNOTEL | 0 | 5150 | 04-26 | N/A | 3 | N/A | N/A | N/A | N/A | ||
| TOUCHET #2 | 2 | 5530 | 04-26 | 14.3 | 55 % | 26.1 | 34 | 42 % | 60 % | 47 % | |
| MILK SHAKES SNOTEL | 0 | 5600 | 04-26 | 31.9 | 77 % | 41.5 | -- | -- | 85 % | 74 % | |
| SPRUCE SPRINGS SNOTEL | 6 | 5700 | 04-26 | 0.0 | 0 % | 8.1 | 0 | -- % | 0 % | 0 % | |
| WOLFCREEK SNOTEL | 1 | 5700 | 04-26 | 3.3 | 33 % | 10.0 | 11 | 30 % | 28 % | 21 % | |
| MOSS SPRINGS SNOTEL | 0 | 5850 | 04-26 | 16.5 | 78 % | 21.1 | 40 | 41 % | 72 % | 69 % | |
| ANEROID LAKE NO 2 SNOTEL | 0 | 7300 | 04-26 | 18.2 | 71 % | 25.8 | 48 | 38 % | 98 % | 71 % | |
| MT HOWARD SNOTEL | 0 | 7910 | 04-26 | 14.0 | 77 % | 18.1 | 165 | 8 % | 81 % | 77 % | |
| Observed Basin Average | 69 % | ||||||||||
| 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. | |||||||||||
