NIDIS Weekly Climate, Water and Drought Assessment Summary. Upper Colorado River Basin November 22, 2011

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Transcription:

NIDIS Weekly Climate, Water and Drought Assessment Summary Upper Colorado River Basin November 22, 2011

PrecipitaEon and Snowpack Fig. 1: November month to date precipitaeon in inches. Fig. 2: November 13 19 precipitaeon in inches. In November so far, generous amounts of precipitaeon have fallen throughout the Upper Colorado River Basin (UCRB, Fig. 1). The higher elevaeons across the Upper and Lower Green River basins and in the northern mountains of Colorado have received over 1 inch month to date, with some areas seeing between 2 and 4 inches. Parts of Utah just south of the Duchesne River, regions around the Four Corners, and much of the northeast plains of CO have have received between a quarter inch and half inch of precipitaeon month todate. The drought stricken southeast CO has received over a half inch to an inch of beneficial moisture since the beginning of the month. Last week, most of the lower elevaeons in the UCRB received less than a tenth of an inch of moisture (Fig. 2). The higher elevaeons conenued to receive more precipitaeon though, with accumulaeons between a quarter inch and 2 inches. The Front Range and plains of Colorado received liule to no precipitaeon for the week. The San Luis Valley also received liule to no precipitaeon last week.

Fig. 3: SNOTEL WYTD precipitaeon perceneles (50% is median, 21 30% is Drought Monitor s D0 category). Fig. 4: San Juan WYTD snow water equivalent accumulaeon (black line) compared to average (green) and last year (teal). Water year to date (WYTD), SNOTEL precipitaeon perceneles are in the near to above average range throughout most of the UCRB (Fig. 3). SNOTEL sites in the Upper Green River basin and in the northern and central mountains of CO range from around the 50 th to the 80 th perceneles. The southern mountains of CO and the mountains in northeast UT have already seen excellent precipitaeon accumulaeons WYTD, with many sites currently near or above the 90 th percenele. Around the San Juan River basin (in the Four Corners region), snow water equivalent has been tracking near average since the beginning of the water year (Fig. 4). Several early snow events quickly melted down, but since the end of October, snowpack has been steadily accumulaeng in the basin. Though current snowpack is just slightly below average, the current accumulaeons are well above the minimum year and also above last year s accumulaeons.

Streamflow As of November 20 th, 89% of the USGS streamgages in the UCRB recorded normal (25 th 75 th percenele) or above normal 7 day average streamflows (Fig. 5). About 13% of the gages in the basin are recording much above normal flows, while 10% of the gages in the basin are recording below normal flows. Most of the gages recording below normal flows are located in the southern part of the basin (in the San Juan basin). Higher flows are currently being observed in the Upper and Lower Green River basins in WY and UT. Key gages on the Colorado River near the CO UT state line and the San Juan River near Bluff, UT are currently recording near normal flows at the 52 nd and 34 th perceneles, respecevely (Fig. 6). The Green River gage at Green River, UT is reporeng above normal flows at the 83 rd percenele. Fig. 5: 7 day average discharge compared to historical discharge for November 20 th. Fig. 6: USGS 7 day average discharge over Eme at the CO UT stateline (top), Green River, UT (middle) and Bluff, UT (bouom).

Water Supply and Demand Last week, near average temperatures were seen across much of the UCRB, with some isolated spots of warmer than average temperatures. Slightly warmer than average temperatures were observed along the Front Range with eastern CO experiencing near to warmer than average temperatures. The VIC model conenues to show dry soil moisture condieons in southeast CO though condieons conenue to improve (Fig. 7). Dry soil condieons are showing up in UT around the Colorado River valley. Soil moisture condieons have improved in Sweetwater County, WY and are now near normal. Wet soils can be seen in the northern CO mountains and eastward. All of the major reservoirs above Lake Powell are near or above their November averages. Most reservoirs have only seen minor drops in storage volumes for the month, with the excepeon of Lake Granby and Green Mountain which have seen relaevely larger decreases. Aside from Lake Granby and Navajo, all of the reservoirs are higher than they were last year at this Eme. Lake Powell is currently at 89% of average and 70% of capacity, compared to 62% of capacity one year ago. PrecipitaEon Forecast As the most recent disturbance exits the region, dry and warm condieons associated with a high pressure system will prevail over the UCRB from now to Thanksgiving. The next disturbance to bring moisture to the basin will arrive on Friday and quickly pass through. PrecipitaEon will mostly be in the form of snow showers for the higher elevaeons in the northern part of the basin, though accumulaeons are expected to be light (Fig. 8). This weekend will see the return of dry and warm condieons across the UCRB. Dry condieons will prevail east of the ConEnental Divide, with eastern CO and the Front Range expected to see liule or no precipitaeon for the week.

Fig. 7: VIC soil moisture perceneles as of November 20 th. Fig. 8: HPC QuanEtaEve PrecipitaEon Forecast (QPF) through 12Z Saturday.

Drought and Water Discussion Drought categories and their associated perceneles Fig. 9: November 15th release of U.S. Drought Monitor for the UCRB Status quo is recommended for the UCRB and across the rest of Colorado in the most current depiceon of the U.S. Drought Monitor (USDM) map (Fig. 9). Areas currently experiencing D0 or greater received liule to no precipitaeon last week, so no improvements are warranted. Dry periods during this Eme of year are normal for these regions. In addieon, nearby snowpack is in good condieon, soil moisture condieons conenue to improve, and streamflows are virtually unchanged. Therefore, degradaeons are not needed at this Eme.