Oceanic Influence on Global Hydrologic Cycle Observed from Space
The divergence of moisture transport integrated over the depth of the atmosphere over global oceans show similar geographic distribution as the surface fresh water flux (evaporationprecipitation). The temporal variations of the two terms also agree, from intraseasonal to interannual time scales, at...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.379.9234 2023-05-15T17:31:46+02:00 Oceanic Influence on Global Hydrologic Cycle Observed from Space W. Timothy Liu Xiaosu Xie Wenqing Tang The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.379.9234 http://airsea-www.jpl.nasa.gov/publication/paper/Liu-etal-2005-igarss.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.379.9234 http://airsea-www.jpl.nasa.gov/publication/paper/Liu-etal-2005-igarss.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://airsea-www.jpl.nasa.gov/publication/paper/Liu-etal-2005-igarss.pdf text ftciteseerx 2016-09-18T00:17:46Z The divergence of moisture transport integrated over the depth of the atmosphere over global oceans show similar geographic distribution as the surface fresh water flux (evaporationprecipitation). The temporal variations of the two terms also agree, from intraseasonal to interannual time scales, at selected locations. These two forcing terms were found to lead ocean surface salinity changes by 90 ° as expected. The interannual anomalies of the hydrologic parameters in the high latitude regions of North American and Eurasia are found the be opposite in phase, and their differences are found to have significant correlation with the moisture transport in the North Atlantic, suggesting N. Atlantic moisture transport is a bridge to the opposing hydrologic phases of the two continents. 1 Text North Atlantic Unknown |
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English |
description |
The divergence of moisture transport integrated over the depth of the atmosphere over global oceans show similar geographic distribution as the surface fresh water flux (evaporationprecipitation). The temporal variations of the two terms also agree, from intraseasonal to interannual time scales, at selected locations. These two forcing terms were found to lead ocean surface salinity changes by 90 ° as expected. The interannual anomalies of the hydrologic parameters in the high latitude regions of North American and Eurasia are found the be opposite in phase, and their differences are found to have significant correlation with the moisture transport in the North Atlantic, suggesting N. Atlantic moisture transport is a bridge to the opposing hydrologic phases of the two continents. 1 |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
W. Timothy Liu Xiaosu Xie Wenqing Tang |
spellingShingle |
W. Timothy Liu Xiaosu Xie Wenqing Tang Oceanic Influence on Global Hydrologic Cycle Observed from Space |
author_facet |
W. Timothy Liu Xiaosu Xie Wenqing Tang |
author_sort |
W. Timothy Liu |
title |
Oceanic Influence on Global Hydrologic Cycle Observed from Space |
title_short |
Oceanic Influence on Global Hydrologic Cycle Observed from Space |
title_full |
Oceanic Influence on Global Hydrologic Cycle Observed from Space |
title_fullStr |
Oceanic Influence on Global Hydrologic Cycle Observed from Space |
title_full_unstemmed |
Oceanic Influence on Global Hydrologic Cycle Observed from Space |
title_sort |
oceanic influence on global hydrologic cycle observed from space |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.379.9234 http://airsea-www.jpl.nasa.gov/publication/paper/Liu-etal-2005-igarss.pdf |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
http://airsea-www.jpl.nasa.gov/publication/paper/Liu-etal-2005-igarss.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.379.9234 http://airsea-www.jpl.nasa.gov/publication/paper/Liu-etal-2005-igarss.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766129509875056640 |