The Summertime Atmospheric Hydrologic Cycle over the Southwestern United StatesSource: Journal of Hydrometeorology:;2004:;Volume( 005 ):;issue: 004::page 679DOI: 10.1175/1525-7541(2004)005<0679:TSAHCO>2.0.CO;2Publisher: American Meteorological Society
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 related to advection from the Gulf of Mexico. The low-level moisture, supplied both by evaporation and advection, is carried aloft primarily by convection (as opposed to large-scale vertical velocities), which then feeds both the precipitation and large-scale divergence fields. The large-scale divergence augments the anticyclonic circulation of moisture aloft, resulting in enhanced exiting fluxes over the Great Plains. A new metric for measuring recycling of moisture in convective semiarid areas is introduced; this metric is designed to better capture the importance of evaporative processes for supporting regional precipitation in these types of environments. Using this metric, it is shown that about 70%?90% of the area-averaged precipitation is the result of evaporative processes, while the remaining 10%?30% is related to low-level convergence of moisture.
|
Collections
Show full item record
contributor author | Anderson, Bruce T. | |
contributor author | Kanamaru, Hideki | |
contributor author | Roads, John O. | |
date accessioned | 2017-06-09T16:17:42Z | |
date available | 2017-06-09T16:17:42Z | |
date copyright | 2004/08/01 | |
date issued | 2004 | |
identifier issn | 1525-755X | |
identifier other | ams-65197.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4206395 | |
description 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 related to advection from the Gulf of Mexico. The low-level moisture, supplied both by evaporation and advection, is carried aloft primarily by convection (as opposed to large-scale vertical velocities), which then feeds both the precipitation and large-scale divergence fields. The large-scale divergence augments the anticyclonic circulation of moisture aloft, resulting in enhanced exiting fluxes over the Great Plains. A new metric for measuring recycling of moisture in convective semiarid areas is introduced; this metric is designed to better capture the importance of evaporative processes for supporting regional precipitation in these types of environments. Using this metric, it is shown that about 70%?90% of the area-averaged precipitation is the result of evaporative processes, while the remaining 10%?30% is related to low-level convergence of moisture. | |
publisher | American Meteorological Society | |
title | The Summertime Atmospheric Hydrologic Cycle over the Southwestern United States | |
type | Journal Paper | |
journal volume | 5 | |
journal issue | 4 | |
journal title | Journal of Hydrometeorology | |
identifier doi | 10.1175/1525-7541(2004)005<0679:TSAHCO>2.0.CO;2 | |
journal fristpage | 679 | |
journal lastpage | 692 | |
tree | Journal of Hydrometeorology:;2004:;Volume( 005 ):;issue: 004 | |
contenttype | Fulltext |