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Modeling the Hydrologic Cycle:The MC Model Part I-Principles and Description
Hydrologic Cycle MC Model Principles Description
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2009/10/27
This article discusses the joint modeling of surface and groundwater flows by
presenting and describing the MC model. The purpose of this deterministic
physically based model is to simulate the beha...
The aggregate description of semi-arid vegetation with precipitation-generated soil moisture heterogeneity
Biosphere-Atmosphere Transfer Scheme semi-arid vegetation soil moisture
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2009/6/8
Meteorological measurements in the Walnut Gulch catchment in Arizona were used to synthesize a distributed, hourly-average time series of data across a 26.9 by 12.5 km area with a grid resolution of 4...
The FORGEX method of rainfall growth estimation II：Description
rainfall growth rainfall growth curve Focused Rainfall Growth Extension
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2009/5/26
The Focused Rainfall Growth Extension (FORGEX) method produces rainfall growth curves focused on a subject site. Focusing allows the incorporation of rainfall extremes observed regionally while respec...
A stochastic approach for the description of the water balance dynamics in a river basin
water balance dynamics river basin
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2009/5/6
The present paper introduces an analytical approach for the description of the soil water balance dynamics over a schematic river basin. The model is based on a stochastic differential equation where ...
An integrated model for the assessment of global water resources–Part 1：Model description and input meteorological forcing
global water resources Global Soil Wetness Project meteorological forcing
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2009/5/4
To assess global water availability and use at a subannual timescale, an integrated global water resources model was developed consisting of six modules: land surface hydrology, river routing, crop gr...
A simple model for predicting soil temperature in snow-covered and seasonally frozen soil: model description and testing
soil temperature snow mode
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2009/3/6
Microbial processes in soil are moisture, nutrient and temperature dependent and, consequently, accurate calculation of soil temperature is important for modelling nitrogen processes.