WANG Xi, WANG Xiuru, JIA Fangfang, et al. Application of Thornthwaite and Mather Water Balance Model in Runoff Yield Calculation at Watershed Scale[J]. Bulletin of Soiland Water Conservation, 2015, 35(1): 193-198.
DOI:
WANG Xi, WANG Xiuru, JIA Fangfang, et al. Application of Thornthwaite and Mather Water Balance Model in Runoff Yield Calculation at Watershed Scale[J]. Bulletin of Soiland Water Conservation, 2015, 35(1): 193-198. DOI: 10.13961/j.cnki.stbctb.2015.01.036.
Application of Thornthwaite and Mather Water Balance Model in Runoff Yield Calculation at Watershed Scale
[Objective] This paper aims to study the monthly water production to guide water resource management and agriculture irrigation scheduling.[Methods] Per capita water possession is only 290 m3 in Jinan City
which is less than one seventh of the nation's level. So Jinan City is in extreme lack of water resources. By taking Jinyangchuan watershed in southern area of Jinan City as the case research area
this paper estimated the water yield under the assistance of image interpretation of remote sensing(RS) and spatial analysis of geographic information system(GIS). First of all
image preprocessing of TM remote sensing data of 2009 was done under ERDAS IMAGINE 9.1 platform
including image synthesis
mosaic
enhancement and correcting. Seven kinds of land use types were identified through supervised classification
the land use map of study area was produced. Second
the soil map of Jinan was vectorized in ARCGIS 9.3 to get the soil texture map in the study area. Third
this study adopted Thornthwaite and Mather (T-M) water balance model to calculate the water balance
obtained the runoff from various land use-soil texture types and cycle of water deficit
moisture surplus
soil moisture recharge and soil moisture utilization in Jinyangchuan watershed. Finally
the runoff path and sub-watershed were generated with Digital Elevation Model (DEM) in EMS-I.WMS.v8.0 (Watershed Modeling System). Then the sub-watershed map was intersected with land use-soil texture map
runoff yield of every sub-watershed in different hydrological years was calculated using weather data from 1960 to 2 011 and subsequently spatially expressed.[Results] The total annual runoff was 281.0 mm
water yield was 51 million m3 in Jinyangchuan watershed in 2011. In January
March
April
June and October
there was water deficit. In February
November and December the soil water was supplied by precipitation; In May
July to September
there was water surplus. The annual average water yield was separately 83 million m3
48 million m3 and 22 million m3 in wet year
normal flow year and low flow year.[Conclusion] There is water surplus in February
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Related Author
Zhu Ji
Deng Furong
Zhao Chenxu
Liu Xingran
WEI Ya-xing
WANG Li-wen
WANG Yi-mou
LIU Yong-mei
Related Institution
Hebei International Joint Research Center for Remote Sensing of Agricultural Drought Monitoring/School of Land Science and Space Planning, Hebei GEO University
Department of Graduate Student, Changan University, Xian
Department of Environment and Engineering, Changan University, Xian
Department of Geoscience and Country’s Resource, Changan University, Xian
Institute of Hydrology and Water Resources, Tsinghua University