홀로세중기의 전지구기후변화 및 아시아 몬순의 변화

Title
홀로세중기의 전지구기후변화 및 아시아 몬순의 변화
Alternative Title
The change in global cliamte and the Asian Monsoon in the Mid-Holocene (6000 Years BP)
Author(s)
김성중; Thomas J. Crowley; 이방용; 박유민; 석봉출
Publication Year
2005-12-06
Abstract
The most active convection in Asian monsoon areas leads to a transfer of heat and moisture to adjacent lands and largely influences the climate, culture, and economy in those areas [Fein and Stephens, 1987; Ding, 1994; Webster et al., 1998]. There are two phases of the Asian monsoon: wet and dry. The wet phase refers to the rainy season during which warm, moist winds blow to land from tropical oceans, while the dry phase refers to a dry season during which cold and dry air blows from the continents. The inter-annual fluctuation of the monsoon is known to largely influence agriculture. A weak monsoon year (i.e. significantly less total rainfall than normal) is generally associated with low crop yields, while a strong monsoon usually produces abundant crops though too much rain leads to devastating floods.
URI
https://sciwatch.kiost.ac.kr/handle/2020.kiost/31175
Bibliographic Citation
Proceedings of the 4th International Synposium on Terrestrial Environmental Changes in East Eurasia and Adjacent Areas, pp.95 - 100, 2005
Publisher
Korea Institute of Geoscience and Mineral Resources
Type
Conference
Language
English
Publisher
Korea Institute of Geoscience and Mineral Resources
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