Quantification of the upstream-to-downstream influence in the Muskingum method and implications for speedup in parallel computations of river flow-Reference-Cited by-同舟云学术

Quantification of the upstream-to-downstream influence in the Muskingum method and implications for speedup in parallel computations of river flow

Published:2013-05 Issue:5 Volume:49 Page:2783-2800
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Resour. Res.

Author:

David Cédric H.¹²,Yang Zong-Liang¹,Famiglietti James S.²³

Affiliation:

1. Department of Geological Sciences; Jackson School of Geosciences, University of Texas at Austin; Austin Texas USA

2. University of California Center for Hydrologic Modeling, University of California; Irvine California USA

3. Department of Earth System Science; University of California; Irvine California USA

Funder

Interdisciplinary Science Project

U.S. National Aeronautics and Space Administration

University of California Office of the President Multicampus Research Programs

Initiatives which are both gratefully acknowledged

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/wrcr.20250/fullpdf

Reference28 articles.

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2. Balay , S. J. Brown K. Buschelman W. D. Gropp D. Kaushik M. G. Knepley L. C. McInnes B. F. Smith H. Zhang 2012 http://www.mcs.anl.gov/petsc

3. On the subject of a flood propagation computation method (Muskingum method);Cunge;J. Hydraul. Res.,1969

4. RAPID applied to the SIM-France model;David;Hydrol. Processes,2011a

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