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Application of Martinec-rango Model to River Basin in JapanVariables and parameters used in applying the Martinec-Rango model to Japan's Okutadami River basin are given. The calculated inflow for three snowmelt seasons is shown in relation to the observed inflow. When the peak inflow occurs, two values of the calculated and the observed do not coincide with each other. A one day lag can be seen between them. Most periods in the season (except peak stage) exhibited a good agreement.
Document ID
19850014917
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Tshihara, K.
(Science and Technology Agency Tokyo, Japan)
Inoue, M.
(Science and Technology Agency Tokyo, Japan)
Takeda, K.
(Science and Technology Agency Tokyo, Japan)
Date Acquired
August 12, 2013
Publication Date
February 1, 1985
Publication Information
Publication: NASA Goddard Space Flight Center Remote Sensing of Snow and Evapotranspiration
Subject Category
Earth Resources And Remote Sensing
Accession Number
85N23228
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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