globalchange  > 气候变化事实与影响
DOI: 10.1175/JCLI-D-15-0800.1
Scopus记录号: 2-s2.0-85010871721
论文题名:
Seasonal differences in precipitation sensitivity to soil moisture in Bangladesh and surrounding regions
作者: Sugimoto S.; Takahashi H.G.
刊名: Journal of Climate
ISSN: 8948755
出版年: 2017
卷: 30, 期:3
起始页码: 921
结束页码: 938
语种: 英语
Scopus关键词: Atmospheric thermodynamics ; Boundary layers ; Climate models ; Condensation ; Frequency response ; Landforms ; Moisture ; Soils ; Surface measurement ; Troposphere ; Atmosphere-land interactions ; Convective precipitation ; Orographic precipitation ; Planetary boundary layers ; Precipitation intensity ; Regional climate modeling ; Regional model ; Seasonal and diurnal variations ; Soil moisture ; atmosphere-biosphere interaction ; climate modeling ; diurnal variation ; precipitation intensity ; regional climate ; seasonal variation ; soil moisture ; Bangladesh
英文摘要: Precipitation sensitivity to soil moisture and its seasonal and diurnal changes are investigated in Bangladesh and surrounding regions using a regional climate model with a 5-km grid spacing. In the control experiment, soil moisture is calculated by a land surface scheme, and simulated accuracy of seasonal and diurnal variations in precipitation intensity and frequency is capable of assessing the soil moisture impact on precipitation. In sensitivity experiments with wetter land surfaces, daytime precipitation intensity decreases over the southern plains for both the premonsoon and mature monsoon seasons because of the weakening of surface heating and vertical mixing in the planetary boundary layer (PBL). Weakened vertical turbulent flux of moisture reduces condensation heating and upward motion in the mid- and upper troposphere, which suppresses development of convective precipitation. The simulated precipitation intensity response to soil moisture suggests that land surface wetness contributes to the seasonal contrast in observed precipitation intensity (i.e., stronger in the premonsoon than the mature monsoon seasons). Meanwhile, the precipitation frequency response to soil moisture varies with season and by region. Over the southern plains in the wet land surface experiments, daytime precipitation frequency decreases (increases) during the premonsoon (mature monsoon) season compared with the dry land surface experiments, as influenced by seasonal differences in relative humidity and the condensation process in the lower troposphere. Around the northern mountainous area, higher soil moisture increases precipitation frequency regardless of season because of additional water vapor supply from the ground and frequent orographic precipitation forced by the mountainous topography.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/49773
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作者单位: Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan; Department of Geography, Tokyo Metropolitan University, Tokyo, Yokohama, Japan

Recommended Citation:
Sugimoto S.,Takahashi H.G.. Seasonal differences in precipitation sensitivity to soil moisture in Bangladesh and surrounding regions[J]. Journal of Climate,2017-01-01,30(3)
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