Large Uncertainties in Runoff Estimations of GLDAS Versions 2.0 and 2.1 in China

Abstract Gauge observed runoff can reflect influences of both natural hydrological cycle and human intervention. The Global Land Data Assimilation System (GLDAS) 2.0 and 2.1 provide abundant runoff which are useful for water resources assessment in ungauged/poorly gauged regions. However, GLDAS2.0 a...

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Main Authors: Wei Qi, Junguo Liu, Hong Yang, Xueping Zhu, Yong Tian, Xin Jiang, Xu Huang, Lian Feng
Format: Article
Language:English
Published: American Geophysical Union (AGU) 2020-01-01
Series:Earth and Space Science
Subjects:
Online Access:https://doi.org/10.1029/2019EA000829
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spelling doaj-4c6682774be0401c978ca48bab7df75f2020-11-24T21:03:46ZengAmerican Geophysical Union (AGU)Earth and Space Science2333-50842020-01-0171n/an/a10.1029/2019EA000829Large Uncertainties in Runoff Estimations of GLDAS Versions 2.0 and 2.1 in ChinaWei Qi0Junguo Liu1Hong Yang2Xueping Zhu3Yong Tian4Xin Jiang5Xu Huang6Lian Feng7School of Environmental Science and Engineering Southern University of Science and Technology Shenzhen ChinaSchool of Environmental Science and Engineering Southern University of Science and Technology Shenzhen ChinaEawag Swiss Federal Institute of Aquatic Science and Technology Duebendorf SwitzerlandCollege of Water Resources Science and Engineering Taiyuan University of Technology Taiyuan ChinaSchool of Environmental Science and Engineering Southern University of Science and Technology Shenzhen ChinaWater Resources Research Institute of Shandong Province Jinan ChinaBureau of Hydrology (Information Center) Songliao Water Resources Commission Jilin ChinaSchool of Environmental Science and Engineering Southern University of Science and Technology Shenzhen ChinaAbstract Gauge observed runoff can reflect influences of both natural hydrological cycle and human intervention. The Global Land Data Assimilation System (GLDAS) 2.0 and 2.1 provide abundant runoff which are useful for water resources assessment in ungauged/poorly gauged regions. However, GLDAS2.0 and GLDAS2.1 runoff have only been validated and inter‐compared in very limited regions. In this study, they are evaluated and inter‐compared utilizing gauge observation in 11 large river basins in China. Results show their runoff have large uncertainties: absolute values of relative bias (|RB|) being above 39% and Nash‐Sutcliffe efficiency lower than 0.15 on average, but GLDAS2.1 is better. Both of them have large uncertainty in the Tibetan Plateau:|RB|are higher than 40%. The gap between GLDAS runoff and observations could attribute to both GLDAS system uncertainty and the fact that GLDAS does not consider human intervention. Therefore, cautions should be taken when using them in coupled human‐natural systems.https://doi.org/10.1029/2019EA000829ChinaGLDASrunoffthe Tibetan Plateauuncertainty
collection DOAJ
language English
format Article
sources DOAJ
author Wei Qi
Junguo Liu
Hong Yang
Xueping Zhu
Yong Tian
Xin Jiang
Xu Huang
Lian Feng
spellingShingle Wei Qi
Junguo Liu
Hong Yang
Xueping Zhu
Yong Tian
Xin Jiang
Xu Huang
Lian Feng
Large Uncertainties in Runoff Estimations of GLDAS Versions 2.0 and 2.1 in China
Earth and Space Science
China
GLDAS
runoff
the Tibetan Plateau
uncertainty
author_facet Wei Qi
Junguo Liu
Hong Yang
Xueping Zhu
Yong Tian
Xin Jiang
Xu Huang
Lian Feng
author_sort Wei Qi
title Large Uncertainties in Runoff Estimations of GLDAS Versions 2.0 and 2.1 in China
title_short Large Uncertainties in Runoff Estimations of GLDAS Versions 2.0 and 2.1 in China
title_full Large Uncertainties in Runoff Estimations of GLDAS Versions 2.0 and 2.1 in China
title_fullStr Large Uncertainties in Runoff Estimations of GLDAS Versions 2.0 and 2.1 in China
title_full_unstemmed Large Uncertainties in Runoff Estimations of GLDAS Versions 2.0 and 2.1 in China
title_sort large uncertainties in runoff estimations of gldas versions 2.0 and 2.1 in china
publisher American Geophysical Union (AGU)
series Earth and Space Science
issn 2333-5084
publishDate 2020-01-01
description Abstract Gauge observed runoff can reflect influences of both natural hydrological cycle and human intervention. The Global Land Data Assimilation System (GLDAS) 2.0 and 2.1 provide abundant runoff which are useful for water resources assessment in ungauged/poorly gauged regions. However, GLDAS2.0 and GLDAS2.1 runoff have only been validated and inter‐compared in very limited regions. In this study, they are evaluated and inter‐compared utilizing gauge observation in 11 large river basins in China. Results show their runoff have large uncertainties: absolute values of relative bias (|RB|) being above 39% and Nash‐Sutcliffe efficiency lower than 0.15 on average, but GLDAS2.1 is better. Both of them have large uncertainty in the Tibetan Plateau:|RB|are higher than 40%. The gap between GLDAS runoff and observations could attribute to both GLDAS system uncertainty and the fact that GLDAS does not consider human intervention. Therefore, cautions should be taken when using them in coupled human‐natural systems.
topic China
GLDAS
runoff
the Tibetan Plateau
uncertainty
url https://doi.org/10.1029/2019EA000829
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