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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 |
| PRLI1L | 4009-6500 | 15.75 | ----- | 11-15 | 0.00 | 0 % | 0.7 | 2.9 | 0.0 | 0.00 | --- | 0.0 | 0.35 |
| PRLI1U | 6500-10145 | 27.56 | ----- | 11-15 | 0.33 | 14 % | 2.3 | 6.6 | 0.0 | 0.98 | 6553 | 0.3 | 0.95 |
| Simulated Basin Average | 11 % | ||||||||||||
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 |
| IDAHO CITY TB30 | 18 | 3965 | 11-15 | N/A | N/A | N/A | N/A | N/A | N/A | ||
| COZY COVE | 6 | 5380 | 11-15 | 0.1 | 20 % | 0.5 | 0 | -- % | 8 % | 1 % | |
| ATLANTA 3 | 10 | 5500 | 11-15 | N/A | N/A | N/A | N/A | N/A | N/A | ||
| GRAHAM GUARD STATION | 5 | 5690 | 11-15 | 0.1 | 25 % | 0.4 | 0 | -- % | 17 % | 1 % | |
| MORES CREEK SUMMIT SNOTEL | 8 | 6100 | 11-15 | 0.4 | 24 % | 1.7 | 1 | 40 % | 80 % | 1 % | |
| DEADWOOD SUMMIT | 22 | 6860 | 11-15 | 0.5 | 15 % | 3.3 | 1 | 50 % | 62 % | 1 % | |
| BANNER SUMMIT | 0 | 7040 | 11-15 | 0.4 | 21 % | 1.9 | 1 | 40 % | 57 % | 2 % | |
| JACKSON PEAK | 0 | 7070 | 11-15 | 0.2 | 11 % | 1.9 | 0 | -- % | 0 % | 1 % | |
| GALENA | 16 | 7440 | 11-15 | 1.1 | 85 % | 1.3 | 2 | 55 % | 92 % | 7 % | |
| ATLANTA SUMMIT | 15 | 7580 | 11-15 | 0.0 | 0 % | 2.2 | 1 | 0 % | 0 % | 0 % | |
| GALENA SUMMIT | 14 | 8795 | 11-15 | 2.1 | 84 % | 2.5 | 12 | 18 % | 100 % | 10 % | |
| VIENNA MINE | 13 | 8960 | 11-15 | 1.4 | 40 % | 3.5 | 7 | 20 % | 87 % | 4 % | |
| Observed Basin Average | 33 % | ||||||||||
| 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. | |||||||||||
