Surface and subsurface water balance estimation by the groundwater recharge model and a 3-D two-phase flow model/Estimation de bilan hydrologique de surface et de subsurface à l’aide de modèles de recharge de nappe et d’écoulement diphasique 3-D-Reference-Cited by-同舟云学术

Surface and subsurface water balance estimation by the groundwater recharge model and a 3-D two-phase flow model/Estimation de bilan hydrologique de surface et de subsurface à l’aide de modèles de recharge de nappe et d’écoulement diphasique 3-D

Published:2004-04 Issue:2 Volume:49 Page:
ISSN:0262-6667
Container-title:Hydrological Sciences Journal
language:en
Short-container-title:Hydrological Sciences Journal

Author:

Tsutsumi Atsushi¹²³,Jinno Kenji¹²³,Berndtsson Ronny¹²³

Affiliation:

1. a Institute of Environmental Systems, Kyushu University, 6-10-1, Hakozaki, Higashiku, Fukuoka 812-8581, Japan

2. b Institute of Environmental Systems, Kyushu University, 6-10-1, Hakozaki, Higashiku, Fukuoka 812-8581, Japan

3. c Department of Water Resources Engineering, Lund University, Box 118, S-221 00 Lund, Sweden

Publisher

Informa UK Limited

Subject

Water Science and Technology

Link

https://www.tandfonline.com/doi/pdf/10.1623/hysj.49.2.205.34837

Reference19 articles.

1. Anderson, M. P. & Woessner, W. W. (1992)Applied Groundwater Modelling Simulation of Flow and Advective Transport. Academic Press, San Diego, California, USA.

2. Beven, K. (1987) Towards a new paradigm in hydrology. In:Water for the Future: Hydrology in Perspective(Proc. Rome Symp., April, 1987), 393?403. IAHS Publ. 164.

3. Bouwer, H. (1978)Groundwater Hydrology, 299?306. McGraw-Hill, New York, USA.

4. Fukushima, Y. & Suzuki, M. (1987) Long-term and short-term hybrid runoff model for small mountain catchment. Research Report of Water Resources 7, 35?52 (in Japanese).

5. The interception, throughfall and stemflow in a forest in Highland Scotland and the comparison with other upland forests in the U.K.

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