• Title/Summary/Keyword: 기후변동

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Future Projections of Köppen Climate Shifts in the Asia Regions Using A2 Scenario (A2 시나리오를 이용한 아시아 지역 기후대의 변화 전망)

  • Shin, Sang Hoon;Bae, Deg Hyo
    • Journal of Korea Water Resources Association
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    • v.46 no.3
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    • pp.253-265
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    • 2013
  • The objective of this study is to analyse the current climate zone applied by K$\ddot{o}$ppen climate classification and the future climate zone projected by the A2 scenario in Asia regions. The spatial and temporal variations of precipitation and temperature were also analyzed. As regards to the result of analysis on the variation of climate factor, temperature and precipitation will be increasing $4.0^{\circ}C$ and 12% respectively in the 2080s comparing with the reference period (1991~2010). Spatially, the range of temperature increase on the high latitude area is higher than that on the low latitude area. The precipitation will be increasing averagely in the overall area, but the spatial unequal distribution of precipitation will be intensified. At the result of the future climate zone, the area of warm climates will be increasing while the area of cold climates will be decreasing. In 2080s, the temperature will be increasing as much as 7.2% and 1.9% on the Tropical climates and Arid climates respectively, but it will be decreasing as -2.4%, -4.9% and -1.8% on the Warm temperate climates, Cold climates and Polar climates respectively. Furthermore, the part of Savannah climates and Desert climates will be mostly increasing. It is mainly caused by the temperature increase and desertification impact according to global warming.

Review of Trends in Recent Climate Research by Korean Climatologists (최근 한국의 기후학 연구 동향)

  • Lee, Eun-Gul;Lee, Kyoung-Mi;Lee, Seung-Ho
    • Journal of the Korean Geographical Society
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    • v.47 no.4
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    • pp.490-513
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    • 2012
  • This study reviewed recent trends in climate research by Korean climatologists. We analyzed six domestic journals listed in the Korean Citation Index and four international journals listed in the Science Citation Index during 2001-2011. Research on climate change has rapidly increased during the study period and studies on precipitation variability have been given continual attentions among Korean climatologists. In climate change research, meteorologists focused on characteristics, prediction, and causes while geographers were more interested in characteristics and impacts of climate change. In applied climatology and bioclimatology, research on the impacts of climate change on agriculture, livestock, vegetation, and human health has increased under recent climate change. While there has been steady interest in climatography by Korean climatologists, the number of papers has generally decreased over the recent period.

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Climate change effect analysis through meteorological data in the Han river basin (기상자료를 통한 한강 유역의 기후 변화 영향 분석)

  • Yang, Jeong-Seok;Kim, Il-Hwan;Kim, Nam-Ki
    • Proceedings of the Korea Water Resources Association Conference
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    • 2012.05a
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    • pp.352-356
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    • 2012
  • 본 연구는 최근 우리나라 4대강 중 한강의 기후변화로 인한 온도, 상대습도, 강우량의 관측자료를 통해 과거와 최근의 변동특성에 대해서 파악하고자 하였다. 이를 위해 기상청의 관측자료를 활용하였으며 한강의 상, 중, 하류로 나눠서 3개 지점에 대해 선정하였다. 선정 기준은 인위적인 영향을 많이 받는 도시지역을 제외한 도서 지역에 위치한 관측소를 기준으로 선정하였다. 분석을 실시한 항목으로는 최고, 최저, 평균기온 및 상대습도, 연강우량, 일 최고 강우량, 강우 집중률이 있으며 강우 집중률은 강우량에 의한 강우강도의 변동 특성을 파악하기 위해 분석하였다. 과거(~1994)와 최근(1995~2011)의 변동성을 파악하기 위해 각 항목별로 비모수적 검정을 실시하고, 상위 10개를 선정한 자료를 이용하여 분석하였다. 비모수적 검정으로는 Mann-Kendall, Hotelling-Pabst, Sen's Trend Test를 이용하였고, 표준정규변량을 통해 과거와 최근의 경향성을 비교하였다. 연구 지점 중 양평의 평균 기온은 상위 10개 중 9개가 최근 자료에서 선정되었고 경향성의 유의수준도 더 높게 나타났다. 최저 상대습도는 과거에 비해 최근에 더 높은 유의수준의 하강하는 경향성을 가지는 것으로 나타나, 기후변화로 인한 지구온난화가 진행되고 있다는 것을 보여주고 있다. 연강수량은 최근 자료에 상위 8개가 나타났고, 표준정규변량 또한 높은 유의수준을 가지며 증가하는 것으로 나타났다. 일 최고 강수량, 강우집중률 또한 상위 10개 관측자료 중 1995년 이후 7개가 관측되었고, 이는 강우강도가 증가하는 것으로 판단할 수 있다. 상대습도의 경우 평균 및 최소 상대습도에서 2개가 관측 되어 기온은 상승하고 강우는 집중되는 반면 상대습도는 온도의 영향 이외에도 낮아지는 경향을 보여 오난해지는 가운데 건조해지는 경향을 보임을 알 수 있었다.

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The Impact of the Oceanic Biological Pump on Atmospheric CO2 and Its Link to Climate Change (해양 생물 펌프가 대기 중 이산화탄소에 미치는 영향 그리고 기후 변동과의 연관성)

  • Kwon, Eun Young;Cho, Yang-Ki
    • The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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    • v.18 no.4
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    • pp.266-276
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    • 2013
  • The ocean is the largest reservoir of carbon in the climate system. Atmospheric $CO_2$ is efficiently transferred to the deep ocean by a process called the biological carbon pump: photosynthetic fixation of $CO_2$ at the sea surface and remineralization of sinking organic carbon at depths are main causes for the vertical contrast of carbon in the ocean. The sequestered carbon to the deep ocean returns to the sea surface by ocean circulation. Part of the upwelled $CO_2$ leaks into the atmosphere through air-sea gas exchange. It has been suggested that the air-sea partitioning of carbon has varied in concert with the glacial-interglacial climate variations, due partly to changes in ocean circulation. In this review paper, we briefly summarize key concepts of the oceanic carbon pump. We also discuss the response of the air-sea carbon partitioning to change in ocean circulation in the context of the glacial-interglacial climate change.

Sensitive analysis of river geometry under various flow conditions in South Han River using GSTARS model (GSTARS 모형을 이용한 한강 상류부에서 유량변동에 따른 하상변동 민감도 분석)

  • Ahn, Jungkyu;Lee, Jong Mun;Kim, Young Do;Kang, Boosik
    • Journal of Korea Water Resources Association
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    • v.49 no.4
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    • pp.347-359
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    • 2016
  • Flow input from the basin will not remain the same as before due to climate changes. Since the predictions on river discharge due to climate change is given by scenarios, various discharge scenarios were prepared in this study. For a long term and reach prediction, semi-two dimensional sediment transport model, GSTARS, was used. The flood water surface elevations predicted by GSTARS model were analysed statistically and it was concluded that the model is applicable for the South Han River. Three stream tubes is the most suitable to simulate two dimensional river geometric change River geometric changes. For sediment load computation, Ackers and White equation and Yang equation were resonable. River will become narrower regardless of discharge variation, more discharge results in deeper channel.