Streamflow Simulation for the Yellow River Basin Using RIEMS and LRM

ZHANG Jingyong; DONG Wenjie; FU Congbin; WU Lingyun; XIONG Zhe; MA Jun; ZHANG Kejia

doi:10.1007/BF02690799

Impact Factor: 5.8

Volume 20 Issue 3

May 2003

Article Contents

Article > ADVANCES IN ATMOSPHERIC SCIENCES > 2003 > 20(3): 415-424

Streamflow Simulation for the Yellow River Basin Using RIEMS and LRM

1.
Global Change System for Analysis, Research and Training Regional Center for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,Global Change System for Analysis, Research and Training Regional Center for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,Global Change System for Analysis, Research and Training Regional Center for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,Global Change System for Analysis, Research and Training Regional Center for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,Global Change System for Analysis, Research and Training Regional Center for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,Hydrological Bureau, Yellow River Conservancy Commission, Zhengzhou 450000,Hydrological Bureau, Yellow River Conservancy Commission, Zhengzhou 450000

doi: 10.1007/BF02690799

Abstract
References
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Abstract:
The streamflow over the Yellow River basin is simulated by using the high-resolution RegionalIntegrated Environmental Model System (RIEMS), and an off-line Large-scale Routing Model (LRM).The RIEMS was designed and has been developed by the Global Change System for Analysis, Researchand Training Regional Center for Temperate East Asia (START/TEA) since 1991 and has a good capabilityto simulate the regional climate of East Asia. The LRM is based on the assumption of linearity and timeinvariance and can calculate the horizontal travel of water. The RIEMS-LRM allows the direct comparisonof predicted and observed streamflow data for large-scale rivers. The application of the RIEMS-LRM tothe upper reaches of the Yellow River verifies that the coupled model system has the capability to simulatethe streamflow over a large-scale river. Furthermore, the paper discusses the reasons leading to simulation errors.
- RIEMS,
- LRM,
- Yellow River,
- streamflow
References

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Manuscript History

Manuscript received: 10 May 2003

Manuscript revised: 10 May 2003

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Streamflow Simulation for the Yellow River Basin Using RIEMS and LRM

1. Global Change System for Analysis, Research and Training Regional Center for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,Global Change System for Analysis, Research and Training Regional Center for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,Global Change System for Analysis, Research and Training Regional Center for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,Global Change System for Analysis, Research and Training Regional Center for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,Global Change System for Analysis, Research and Training Regional Center for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,Hydrological Bureau, Yellow River Conservancy Commission, Zhengzhou 450000,Hydrological Bureau, Yellow River Conservancy Commission, Zhengzhou 450000

Manuscript received: 2003-05-10
Manuscript revised: 2003-05-10

Abstract: The streamflow over the Yellow River basin is simulated by using the high-resolution RegionalIntegrated Environmental Model System (RIEMS), and an off-line Large-scale Routing Model (LRM).The RIEMS was designed and has been developed by the Global Change System for Analysis, Researchand Training Regional Center for Temperate East Asia (START/TEA) since 1991 and has a good capabilityto simulate the regional climate of East Asia. The LRM is based on the assumption of linearity and timeinvariance and can calculate the horizontal travel of water. The RIEMS-LRM allows the direct comparisonof predicted and observed streamflow data for large-scale rivers. The application of the RIEMS-LRM tothe upper reaches of the Yellow River verifies that the coupled model system has the capability to simulatethe streamflow over a large-scale river. Furthermore, the paper discusses the reasons leading to simulation errors.

Keywords: