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Browsing by Author "Xie, Xiaosu"

Browsing by Author "Xie, Xiaosu"

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  • Liu, W. Timothy; Xie, Xiaosu (Pasadena, CA : Jet Propulsion Laboratory, National Aeronautics and Space Administration, 2006., 2006-04-24)
    The approximate balance of the mass change rate measured by the Gravity Recovery and Climate Experiment (GRACE) with the moisture influx across the entire coastline less climatological river discharge for South America ...
  • Liu, W. Timothy; Xie, Xiaosu (Pasadena, CA : Jet Propulsion Laboratory, National Aeronautics and Space Administration, 2014, 2014-09-01)
    We have developed and validated a statistical model to estimate the fugacity (or partial pressure) of carbon dioxide (CO2) at sea surface (pCO2sea) from space-based observations of sea surface temperature (SST), chlorophyll, ...
  • Liu, W. Timothy; Xie, Xiaosu; Niiler, Pearn P. (American Meteorological Society, 2007-03-15)
    Many years of high-resolution measurements by a number of space-based sensors and from Lagrangian drifters became available recently and are used to examine the persistent atmospheric imprints of the semipermanent meanders ...
  • Xie, Xiaosu; Liu, W. Timothy; Tang, Benyang (Elsevier Inc, 2007)
    An improved algorithm is developed based on support vector regression (SVR) to estimate horizonal water vapor transport integrated through the depth of the atmosphere (Θ) over the global ocean from observations of surface ...
  • Liu, W. Timothy; Xie, Xiaosu; Tang, Wenqing; Zlotnicki, Victor (American Geophysical Union, 2006-04-27)
    The mass change of South America (SA) continent measured by the Gravity Recovery and Climate Experiment (GRACE) imposes a constraint on the uncertainties in estimating the annual variation of rainfall measured by Tropical ...
  • Liu, W. Timothy; Tang, Wenqing; Xie, Xiaosu (Pasadena, CA: Jet Propulsion Laboratory, National Aeronautics and Space Administration, 2016, 2016-07-10)
    Ocean surface wind (U) is air in motion and stress (τ) is the turbulent transport of momentum between the ocean and the atmosphere. While the strong wind of a tropical cyclone (TC) causes destruction at landfall, it is the ...