|
|
| 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 |
| TOTW1L | 160-3500 | 393.66 | ----- | 05-01 | 0.00 | N/A | 0.0 | 0.0 | 0.0 | 0.00 | --- | 0.2 | 0.03 |
| TOTW1U | 3500-7874 | 393.66 | ----- | 05-01 | 23.89 | 104 % | 22.9 | 58.8 | 1.4 | 0.50 | 3993 | 22.1 | 0.75 |
| Simulated Basin Average | 104 % | ||||||||||||
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 |
| PEPPER CREEK SNOTEL | 12 | 2140 | 05-01 | N/A | 2 | N/A | N/A | N/A | N/A | ||
| CALAMITY | 18 | 2470 | 05-01 | 0.8 | 114 % | 0.7 | 0 | -- % | N/A | N/A | |
| SPIRIT | 0 | 3120 | 05-01 | 0.0 | 0 % | 2.0 | 0 | -- % | 0 % | 0 % | |
| JUNE LAKE SNOTEL | 4 | 3340 | 05-01 | 35.8 | 99 % | 36.1 | 67 | 53 % | 74 % | 88 % | |
| SPENCER MEADOWS SNOTEL | 10 | 3400 | 05-01 | 12.4 | 52 % | 24.0 | 27 | 46 % | 43 % | 40 % | |
| LONE PINE SNOTEL | 6 | 3800 | 05-01 | 40.1 | 108 % | 37.0 | 74 | 54 % | 85 % | 102 % | |
| SHEEP CANYON SNOTEL | 0 | 4030 | 05-01 | 34.2 | 103 % | 33.2 | 69 | 50 % | 79 % | 94 % | |
| SURPRISE LAKES SNOTEL | 20 | 4250 | 05-01 | 40.8 | 94 % | 43.4 | 86 | 47 % | 79 % | 86 % | |
| SWIFT CREEK SNOTEL | 1 | 4440 | 05-01 | 84.7 | 125 % | 67.6 | 152 | 56 % | 91 % | 123 % | |
| Observed Basin Average | 102 % | ||||||||||
| 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. | |||||||||||
