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Record #119122:

Computation of a snowpack-loss component for a water-budget model for the San Juan aquifer basin in New Mexico and Colorado / Scott D. Waltemeyer, John M. Kernodle.

Title: Computation of a snowpack-loss component for a water-budget model for the San Juan aquifer basin in New Mexico and Colorado / Scott D. Waltemeyer, John M. Kernodle.
Author(s): Waltemeyer, Scott D.
Kernodle, John M.
Date: 1992.
In: Western Snow Conference. Proceedings. (1992.), Vol. 60th Annual Meeting (1992)
Abstract: Precipitation component of model uses average-basin mean annual winter precipitation (May to September precipitation is considered lost to evapotranspiration). Streamflow component is derived by regression relations based on drainage area and mean annual winter precipitation for three physiographic regions. Snowpack-loss component is derived by defining relation of peak snowpack water content to total precipitation for given altitude. Snowpack loss ranged from 27 to 57% for altitudes of 3048 and 2286 m, respectively.
Notes:

Western Snow Conference. Proceedings. Vol. 60th Annual Meeting :141-145 (1992).

Keywords: 556 -- Hydrology.
556.51 -- River basins and watersheds.
551.579.2 -- Water supply from snow.
551.578.462 -- Snow cover, ablation.
551.578.46 -- Snow cover and snow patches.
519.673 -- Modelling.
E11 -- Glaciology: glaciohydrology.
(73) -- United States.
(78) -- Western states.
SPRI record no.: 119122

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245 10 ‡aComputation of a snowpack-loss component for a water-budget model for the San Juan aquifer basin in New Mexico and Colorado /‡cScott D. Waltemeyer, John M. Kernodle.
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500 ## ‡aWestern Snow Conference. Proceedings. Vol. 60th Annual Meeting :141-145 (1992).
520 3# ‡aPrecipitation component of model uses average-basin mean annual winter precipitation (May to September precipitation is considered lost to evapotranspiration). Streamflow component is derived by regression relations based on drainage area and mean annual winter precipitation for three physiographic regions. Snowpack-loss component is derived by defining relation of peak snowpack water content to total precipitation for given altitude. Snowpack loss ranged from 27 to 57% for altitudes of 3048 and 2286 m, respectively.
650 07 ‡a556 -- Hydrology.‡2udc
650 07 ‡a556.51 -- River basins and watersheds.‡2udc
650 07 ‡a551.579.2 -- Water supply from snow.‡2udc
650 07 ‡a551.578.462 -- Snow cover, ablation.‡2udc
650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡aE11 -- Glaciology: glaciohydrology.‡2local
651 #7 ‡a(73) -- United States.‡2udc
651 #7 ‡a(78) -- Western states.‡2udc
700 1# ‡aKernodle, John M.
773 0# ‡7nnas ‡tWestern Snow Conference. Proceedings. ‡gVol. 60th Annual Meeting (1992) ‡wSPRI-26976
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