Editorial Type:
Article
Article Type:
Research Article

Effect of Seasonality of Snow Accumulation and Melt on Snow Surface Energy Exchanges at a Continental Alpine Site

Donald W. Cline Institute of Arctic and Alpine Research, University of Colorado, Boulder, Colorado

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Print Publication:
01 Jan 1997
DOI:
https://doi.org/10.1175/1520-0450(1997)036<0032:EOSOSA>2.0.CO;2
Page(s):
32–51
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Abstract

Snow surface energy exchanges and snowmelt were measured during the 1994 and 1995 snowmelt seasons at an alpine site in the Colorado Front Range (3517 m MSL, 40°03′N, 105°35′W). Following a maximum accumulation of 0.49-m snow water equivalence (SWE), the 1994 snowmelt season began on 5 May and lasted 32 days until 6 June. In contrast, the 1995 maximum accumulation of 1.31-m SWE did not occur until 1 June, and the snowmelt season lasted 45 days until July 16. Thus, a nearly threefold larger snowpack ablated in only 41% more time in the later 1995 snowmelt season. In 1994, net radiation accounted for 75% of the energy available to melt snow, and sensible and latent heat fluxes accounted for the remaining 25%. During the 1995 snowmelt season the mean air temperature was warmer (+1.3°C) and the mean specific humidity was greater (+0.6 g kg−1) than during the 1994 snowmelt season. As a result, in 1995, sensible and latent heat fluxes accounted for 54% of the energy for snowmelt and net radiation accounted for only 46%. Midday maximum snowmelt rates were approximately equal in 1994 and 1995; the overall more rapid 1995 melt rate was due to the frequent occurrence of nocturnal melting, which did not occur in 1994. The large differences between these two snowmelt seasons provide analogies for understanding regional variability of snowmelt processes and for understanding alpine snowmelt response to climate variability and change.

Corresponding author address: Dr. Donald W. Cline, National Operational Hydrologic Remote Sensing Center, Office of Hydrology, National Weather Service, NOAA, 1735 Lake Drive West, Chanhassen, MN 55317-8582.

Abstract

Snow surface energy exchanges and snowmelt were measured during the 1994 and 1995 snowmelt seasons at an alpine site in the Colorado Front Range (3517 m MSL, 40°03′N, 105°35′W). Following a maximum accumulation of 0.49-m snow water equivalence (SWE), the 1994 snowmelt season began on 5 May and lasted 32 days until 6 June. In contrast, the 1995 maximum accumulation of 1.31-m SWE did not occur until 1 June, and the snowmelt season lasted 45 days until July 16. Thus, a nearly threefold larger snowpack ablated in only 41% more time in the later 1995 snowmelt season. In 1994, net radiation accounted for 75% of the energy available to melt snow, and sensible and latent heat fluxes accounted for the remaining 25%. During the 1995 snowmelt season the mean air temperature was warmer (+1.3°C) and the mean specific humidity was greater (+0.6 g kg−1) than during the 1994 snowmelt season. As a result, in 1995, sensible and latent heat fluxes accounted for 54% of the energy for snowmelt and net radiation accounted for only 46%. Midday maximum snowmelt rates were approximately equal in 1994 and 1995; the overall more rapid 1995 melt rate was due to the frequent occurrence of nocturnal melting, which did not occur in 1994. The large differences between these two snowmelt seasons provide analogies for understanding regional variability of snowmelt processes and for understanding alpine snowmelt response to climate variability and change.

Corresponding author address: Dr. Donald W. Cline, National Operational Hydrologic Remote Sensing Center, Office of Hydrology, National Weather Service, NOAA, 1735 Lake Drive West, Chanhassen, MN 55317-8582.

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