A Transfer Function Between Line‐of‐Sight Gravity Difference and GRACE Intersatellite Ranging Data and an Application to Hydrological Surface Mass Variation-Reference-Cited by-同舟云学术

A Transfer Function Between Line‐of‐Sight Gravity Difference and GRACE Intersatellite Ranging Data and an Application to Hydrological Surface Mass Variation

Published:2018-10 Issue:10 Volume:123 Page:9186-9201
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Ghobadi‐Far Khosro¹^ORCID,Han Shin‐Chan¹^ORCID,Weller Steven²^ORCID,Loomis Bryant D.³,Luthcke Scott B.³,Mayer‐Gürr Torsten⁴,Behzadpour Saniya⁴⁵

Affiliation:

1. School of Engineering University of Newcastle Callaghan New South Wales Australia

2. School of Electrical Engineering and Computing University of Newcastle Callaghan New South Wales Australia

3. Geodesy and Geophysics Laboratory NASA Goddard Space Flight Center Greenbelt MD USA

4. Institute of Geodesy Graz University of Technology Graz Austria

5. Institute of Geodesy Leibniz University of Hanover Hannover Germany

Funder

University of Newcastle Australia

Australian Research Council

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB016088

Reference53 articles.

1. Global Evaluation of the ISBA-TRIP Continental Hydrological System. Part I: Comparison to GRACE Terrestrial Water Storage Estimates and In Situ River Discharges

2. Bettadpur S.(2012).Gravity Recovery and Climate Experiment UTCSR Level‐2 Processing Standards Document for Level‐2 Product Release 0005. Center for Space Research. University of Texas Austin.

3. Continental runoff dynamics in the Community Climate System Model 2 (CCSM2) control simulation

4. Continental Water Storage Changes from GRACE Line-of-Sight Range Acceleration Measurements

5. Global Evaluation of the ISBA-TRIP Continental Hydrological System. Part II: Uncertainties in River Routing Simulation Related to Flow Velocity and Groundwater Storage

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