Disturbances of temperature-depth profiles due to surface climate change and subsurface water flow: 1. An effect of linear increase in surface temperature caused by global warming and urbanization in the Tokyo metropolitan area, Japan

被引:139
作者
Taniguchi, M [1 ]
Shimada, J
Tanaka, T
Kayane, I
Sakura, Y
Shimano, Y
Dapaah-Siakwan, S
Kawashima, S
机构
[1] Nara Med Educ, Dept Earth Sci, Nara 6308528, Japan
[2] Univ Tsukuba, Inst Geosci, Tsukuba, Ibaraki 3058571, Japan
[3] Aichi Univ, Grad Sch, Nagoya, Aichi 4700296, Japan
[4] Chiba Univ, Dept Earth Sci, Chiba 2638522, Japan
[5] Bunsei Coll, Utsunomiya, Tochigi 3200058, Japan
[6] Inst Water Resources, Accra, Ghana
[7] Inst Civil Engn Tokyo Metropolitan Govt, Dept Geosci, Tokyo 1360075, Japan
关键词
D O I
10.1029/1999WR900009
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
A series of type curves is presented for evaluating vertical groundwater fluxes under the condition of a linear increase in surface temperature. The depths of minimum groundwater temperature in the temperature-depth profiles indicate the magnitude of the downward groundwater flux. The type curve method has been applied to the subsurface thermal regime observed in Tokyo metropolitan area, Japan, to estimate the vertical groundwater fluxes under the condition of surface warming caused by global warming and urbanization. The groundwater fluxes obtained from the type curves and the depths of minimum groundwater temperature agree well with the values obtained from the other studies in the Tokyo metropolitan area. The inversion due to the surface warming could be a good tracer to detect the groundwater flow system.
引用
收藏
页码:1507 / 1517
页数:11
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