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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 |
| TEAI1XD | 4994-6500 | 393.66 | ----- | - | N/A | N/A | N/A | N/A | N/A | 0.00 | --- | N/A | N/A |
| TEAI1XL | 4994-6500 | 393.66 | ----- | 05-22 | 0.00 | N/A | 0.0 | 0.0 | 0.0 | 0.00 | --- | 0.0 | 0.00 |
| TEAI1XU | 6500-10148 | 27.56 | ----- | 05-22 | 2.33 | 33 % | 7.1 | 22.8 | 0.0 | 0.91 | 6647 | 2.6 | 0.18 |
| Simulated Basin Average | 33 % | ||||||||||||
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 |
| PINE CK PASS SNOTEL | 8 | 6720 | 05-23 | 0.0 | 0 % | 0.4 | 0 | -- % | 0 % | 0 % | |
| SNKE R ON JACKSN LK AT DM TB20 | 13 | 6728 | 05-23 | N/A | N/A | N/A | N/A | N/A | N/A | ||
| SNAKE RIVER STATION SNOTEL | 14 | 6920 | 05-23 | 0.0 | 0 % | 0.7 | 0 | -- % | 0 % | 0 % | |
| BASECAMP SNOTEL | 21 | 7030 | 05-23 | N/A | 1.8 | N/A | N/A | N/A | N/A | ||
| GLADE CREEK NR MORAN | 12 | 7040 | 05-23 | N/A | N/A | N/A | N/A | N/A | N/A | ||
| GRASSY LAKE SNOTEL | 10 | 7265 | 05-23 | 0.0 | 0 % | 14.1 | 0 | -- % | 0 % | 0 % | |
| HUCKLEBERRY DIV NR MORAN TB30 | 10 | 7300 | 05-23 | N/A | N/A | N/A | N/A | N/A | N/A | ||
| LEWIS LAKE DIVIDE SNOTEL | 18 | 7860 | 05-23 | 5.8 | 32 % | 18.1 | 11 | 53 % | 19 % | 17 % | |
| PHILLIPS BENCH SNOTEL | 22 | 8200 | 05-23 | 2.8 | 17 % | 16.8 | 6 | 47 % | 14 % | 10 % | |
| GRAND TARGHEE | 6 | 9260 | 05-23 | N/A | 42.4 | N/A | N/A | N/A | N/A | ||
| Observed Basin Average | 17 % | ||||||||||
| 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. | |||||||||||
