Heat Balance and Soil Water Content for Bare Soil Surfaces in the Loess Plateau, China
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- KIMURA Reiji
- Arid Land Research Center, Tottori University
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- LIU Yuanbo
- Graduate School of Environmental Studies, Nagoya University
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- TAKAYAMA Naru
- Arid Land Research Center, Tottori University
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- KAMICHIKA Makio
- Arid Land Research Center, Tottori University
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- MATSUOKA Nobuhiro
- Faculty of Horticulture, Chiba University
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- ZHANG Xingchang
- Institute of Soil and Water Conservation, CAS
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Abstract
Spatial and temporal changes of heat and water balances are crucial for obtaining the greatest benefits from planting to combat desertification in the Loess Plateau of China. We used a three-layer soil model and routine meteorological data from 43 observatories to estimate the heat and water balances of the bare soil surface in this area. The results indicate that the annual mean of the sensible heat flux ranged from 13 Wm-2 to 36 Wm-2, and the annual mean of the latent heat flux was from 14 Wm-2 (179 mmy-1) to 40 Wm-2 (521 mmy-1). Water retention and restriction of evaporation from the soil surface are affected by the yellow loessial soil, including medium loam, light loam, and sandy loam, but not heavy loam. We also compared the distribution of fractional extractable water and of the existing vegetation to reveal the potential vegetation distribution. Finally, we clarified the aridity distribution in the plateau.
Journal
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- Journal of Agricultural Meteorology
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Journal of Agricultural Meteorology 60 (5), 1013-1016, 2005
The Society of Agricultural Meteorology of Japan
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Details 詳細情報について
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- CRID
- 1390282679644632448
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- NII Article ID
- 130006847364
- 40015149554
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- NII Book ID
- AA11530034
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- ISSN
- 18810136
- 00218588
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- NDL BIB ID
- 8546643
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- Text Lang
- en
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- Data Source
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- JaLC
- NDL
- Crossref
- CiNii Articles
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- Abstract License Flag
- Disallowed