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- W2169085749 abstract "Abstract In this paper the authors examine the large-scale summertime hydrologic cycle associated with the northwestern branch of the North American monsoon, centered on the southwestern United States, using a suite of surface-and upper-air-based observations, reanalysis products, and regional model simulations. In general, it is found that on an area-averaged basis, seasonal precipitation is balanced predominantly by evaporation; in addition, this evaporation also supports a net, vertically integrated moisture flux divergence from the region of the same magnitude as the precipitation itself. This vertically integrated large-scale moisture flux divergence is the result of an offsetting balance between convergence of low-level moisture and divergence of moisture aloft (<750 mb). Over the western portion of the domain, most of this low-level moisture convergence is related to advection from the Gulf of California and eastern Pacific; over the eastern portion of the domain, low-level moisture convergence is ..." @default.
- W2169085749 created "2016-06-24" @default.
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- W2169085749 date "2004-08-01" @default.
- W2169085749 modified "2023-09-30" @default.
- W2169085749 title "The Summertime Atmospheric Hydrologic Cycle over the Southwestern United States" @default.
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- W2169085749 doi "https://doi.org/10.1175/1525-7541(2004)005<0679:tsahco>2.0.co;2" @default.
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