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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 |
| VIDO3XL | 856-3799 | 7.87 | ----- | - | N/A | N/A | N/A | N/A | N/A | 0.00 | --- | N/A | N/A |
| VIDO3XM | 3800-5499 | 393.66 | ----- | - | N/A | N/A | N/A | N/A | N/A | 0.00 | --- | N/A | N/A |
| VIDO3XU | 5500-10358 | 393.66 | ----- | - | N/A | N/A | N/A | N/A | N/A | 0.00 | --- | N/A | N/A |
| Simulated Basin Average | N/A | ||||||||||||
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 |
| RAIL ROAD OVERPASS SNOTEL | 22 | 2750 | 01-07 | 0.0 | 0 % | 0.6 | 0 | -- % | 0 % | 0 % | |
| JUMP OFF JOE SNOTEL | 12 | 3500 | 01-07 | 0.8 | 13 % | 6.0 | 1 | 80 % | 100 % | 7 % | |
| DALY LAKE SNOTEL | 21 | 3600 | 01-07 | 1.5 | 19 % | 7.7 | 152 | 1 % | 100 % | 10 % | |
| SANTIAM JUNCTION SNOTEL | 18 | 3750 | 01-07 | 1.2 | 15 % | 7.9 | 6 | 20 % | 100 % | 9 % | |
| BEAR GRASS SNOTEL | 9 | 4720 | 01-07 | N/A | N/A | N/A | N/A | N/A | N/A | ||
| HOGG PASS SNOTEL SNOTEL | 19 | 4760 | 01-07 | 4.5 | 42 % | 10.7 | 18 | 25 % | 100 % | 20 % | |
| ROARING RIVER SNOTEL | 5 | 4900 | 01-07 | 2.8 | 23 % | 12.3 | 161 | 2 % | 100 % | 10 % | |
| HOLLAND MEADOWS SNOTEL | 25 | 4900 | 01-07 | 2.8 | 29 % | 9.8 | 8 | 35 % | 72 % | 16 % | |
| MCKENZIE SNOTEL | 6 | 5000 | 01-07 | 4.7 | 26 % | 18.3 | 20 | 24 % | 100 % | 12 % | |
| IRISH TAYLOR SNOTEL | 11 | 5500 | 01-07 | 5.7 | 37 % | 15.6 | 20 | 29 % | 100 % | 16 % | |
| Observed Basin Average | 27 % | ||||||||||
| 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. | |||||||||||
