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Wiktionary英語版
出典：Wiktionary
throughflow
名詞
throughflow (countable かつ uncountable, 複数形 throughflows)
- (hydrology) The movement of water horizontally beneath the land surface, usually when the soil is completely saturated.
- (hydrology) The movement of an identifiably separate body of water through a larger body (such as a current of fresh water through salt water).
- 2001, Harry L. Bryden, Shiro Imawaki, 6.1: Ocean Heat Transport, Gerold Siedler, John Church, John Gould (editors), Ocean Circulation and Climate: Observing and Modelling the Global Ocean, Harcourt Science and Technology (Academic Press), page 464,
- As for the Pacific, the unknown size of the Indonesian Throughflow complicates quantitative estimates of heat transport divergence in the Indian Ocean. Because the Throughflow entering the Indian Ocean is warm (about 20°C) relative to its temperature as it exits the Indian Ocean across the southern boundary at 32°S, the overall effect of the Throughflow is to lead to an ocean heat transport convergence over the Indian Ocean.
- 2001, Harry L. Bryden, Shiro Imawaki, 6.1: Ocean Heat Transport, Gerold Siedler, John Church, John Gould (editors), Ocean Circulation and Climate: Observing and Modelling the Global Ocean, Harcourt Science and Technology (Academic Press), page 464,
参考
アナグラム
ウィキペディア英語版
出典：Wikipedia
Throughflow
出典:『Wikipedia』 (2011/03/13 22:16 UTC 版)
英語による解説
ウィキペディア英語版からの引用
- 引用
In hydrology, throughflow is the horizontal movement of water in the soil zone. This type of flow must first emerge on land before it enters a body of surface water (stream, lake, pond) to be considered throughflow (as opposed to interflow where the flow enters directly the body of surface water without having first emerged at the surface). Once water infiltrates the soil, it moves downwards under gravity and, because the soil becomes more compact and less permeable with increasing depth, will begin to move sideways at speeds of between 0.005 to 0.3 m/h. Throughflow usually happens when the soil is completely saturated with water. This water then flows underground until it reaches a river, lake, or ocean. The lowest rates of flow occur in heavy clay soils.
- All Rights Reserved, Copyright © Japan Science and Technology Agency
- Wiktionary
- Text is available under Creative Commons Attribution-ShareAlike (CC-BY-SA) and/or GNU Free Documentation License (GFDL).
Weblio英和・和英辞典に掲載されている「Wiktionary英語版」の記事は、Wiktionaryのthroughflow (改訂履歴)の記事を複製、再配布したものにあたり、Creative Commons Attribution-ShareAlike (CC-BY-SA)もしくはGNU Free Documentation Licenseというライセンスの下で提供されています。
- Wikipedia
- Text is available under Creative Commons Attribution-ShareAlike (CC-BY-SA) and/or GNU Free Documentation License (GFDL).
Weblio英和・和英辞典に掲載されている「Wikipedia英語版」の記事は、WikipediaのThroughflow (改訂履歴)の記事を複製、再配布したものにあたり、Creative Commons Attribution-ShareAlike (CC-BY-SA)もしくはGNU Free Documentation Licenseというライセンスの下で提供されています。
