|
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 |
SPEW1L | 594-3500 | 393.66 | ----- | 04-17 | 0.00 | N/A | 0.0 | 0.0 | 0.0 | 0.00 | --- | 0.4 | 0.38 |
SPEW1U | 3500-5427 | 393.66 | ----- | 04-17 | 10.90 | 56 % | 19.5 | 44.8 | 1.2 | 0.63 | 3992 | 8.6 | 0.98 |
Simulated Basin Average | 56 % |
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 |
HUCKLEBERRY CREEK SNOTEL | 12 | 2000 | 04-18 | 0.0 | 0 % | 0.3 | 1 | 0 % | 0 % | 0 % | |
MOWICH SNOTEL | 6 | 3150 | 04-18 | N/A | 0.6 | N/A | N/A | N/A | N/A | ||
COUGAR MOUNTAIN SNOTEL | 16 | 3200 | 04-17 | 0.0 | 0 % | 13.6 | 0 | -- % | 0 % | 0 % | |
LYNN LAKE SNOTEL | 8 | 4000 | 04-18 | 9.9 | 37 % | 26.9 | -- | -- | 83 % | 36 % | |
REX RIVER SNOTEL | 20 | 4000 | 04-18 | 20.5 | 61 % | 33.4 | -- | -- | 89 % | 59 % | |
BURNT MTN SNOTEL | 0 | 4200 | 04-18 | 6.7 | 36 % | 18.7 | 13 | 52 % | N/A | N/A | |
PARADISE SNOTEL | 17 | 5120 | 04-18 | 58.2 | 78 % | 75.0 | 116 | 50 % | 98 % | 76 % | |
CAYUSE PASS SNOTEL | 18 | 5200 | 04-18 | 38.1 | 64 % | 59.2 | 88 | 43 % | 95 % | 64 % | |
MORSE LAKE SNOTEL | 19 | 5400 | 04-18 | 45.1 | 82 % | 54.7 | 90 | 50 % | 96 % | 82 % | |
CORRAL PASS SNOTEL | 17 | 6000 | 04-18 | 24.1 | 66 % | 36.5 | 56 | 43 % | 91 % | 66 % | |
Observed Basin Average | 65 % | ||||||||||
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. |