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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 |
| DWRI1IL | 1445-4500 | 15.75 | ----- | 06-08 | 0.00 | 0 % | 0.0 | 0.3 | 0.0 | 0.00 | --- | 0.0 | 0.00 |
| DWRI1IU | 4500-7392 | 43.31 | ----- | 06-08 | 4.87 | 52 % | 9.4 | 36.1 | 0.3 | 0.16 | 5935 | 1.1 | 0.18 |
| Simulated Basin Average | 52 % | ||||||||||||
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 |
| PIERCE SNOTEL | 4 | 3080 | 06-16 | N/A | N/A | N/A | N/A | N/A | N/A | ||
| SHERWIN | 7 | 3200 | 06-16 | 0.1 | N/A | 0 | 1 | 10 % | N/A | N/A | |
| SHANGHAI SUMMIT | 2 | 4570 | 06-16 | N/A | 0.2 | N/A | N/A | N/A | N/A | ||
| LOLO PASS | 9 | 5240 | 06-15 | 9.1 | 1300 % | 0.7 | -9999 | -- % | N/A | N/A | |
| ELK BUTTE | 0 | 5550 | 06-16 | 0.0 | 0 % | 3.3 | 0 | -- % | 0 % | 0 % | |
| HEMLOCK BUTTE | 0 | 5810 | 06-15 | 0.0 | 0 % | 6.5 | -9999 | -- % | 0 % | 0 % | |
| CRATER MEADOWS | 0 | 5960 | 06-16 | 0.0 | 0 % | 8.7 | 0 | -- % | 0 % | 0 % | |
| HOODOO BASIN SNOTEL | 0 | 6050 | 06-16 | 7.0 | 53 % | 13.1 | -- | -- | 19 % | 17 % | |
| LOST LAKE | 0 | 6110 | 06-16 | 1.7 | 9 % | 19.2 | 2 | 85 % | 3 % | 3 % | |
| COOL CREEK | 0 | 6280 | 06-16 | 5.4 | 26 % | 20.9 | 11 | 49 % | 12 % | 11 % | |
| Observed Basin Average | 20 % | ||||||||||
| Please Note: Snow stations highlighted in light grey are reported as questionable by the reporting agency and are not included in the basin average caclulation. | |||||||||||
| 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. | |||||||||||
