Mountain hydrology of the western United States
نویسندگان
چکیده
C31A-0275.Dozier, J., and T. H. Painter (2004), Multispectral and hyperspectral remotesensing of alpine snow properties, Annu. Rev. Earth Planet. Sci., 32, 465–494, doi:10.1146/annurev.earth.32.101802.120404.Dressler, K. A., G. Leavesley, R. C. Bales, and S. Fassnacht (2004),Streamflow estimation from hydrologic model assimilation of remotelysensed snow information in snowmelt dominated basins, Eos Trans.AGU, 85(47), Fall Meet. Suppl., Abstract C31A-0288.Entekhabi, D. (2005), Estimation of land surface latent heat flux and itsdeterminants based on remotely sensed measurements, Eos Trans. AGU, 86(52), Fall Meet. Suppl., Abstract H14B-01.Fassnacht, S. R., K. A. Dressler, and R. C. Bales (2003), Snow waterequivalent interpolation for the Colorado River Basin from snow tele-metry (SNOTEL) data, Water Resour. Res., 39(8), 1208, doi:10.1029/2002WR001512. 12 of 13W08432BALES ET AL.: MOUNTAIN HYDROLOGY OF THE WESTERN USW08432
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Detection and Attribution of Temperature Changes in the Mountainous Western United States
Large changes in the hydrology of the western United States have been observed since the mid-twentieth century. These include a reduction in the amount of precipitation arriving as snow, a decline in snowpack at low and midelevations, and a shift toward earlier arrival of both snowmelt and the centroid (center of mass) of streamflows. To project future water supply reliability, it is crucial to...
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