第四纪研究
第四紀研究
제사기연구
2009年
6期
1011-1014
,共4页
王会军%王涛%姜大膀%富元海
王會軍%王濤%薑大膀%富元海
왕회군%왕도%강대방%부원해
气候变化%预估%脆弱区
氣候變化%預估%脆弱區
기후변화%예고%취약구
climate change%projection%vulnerable region
从当今国际上不同的气候系统模式模拟的全新世大暖期和末次盛冰期我国气候变化量级和复原资料结果的对比,以及从目前气候变化的趋势(包括温室气体、气温、海洋温度、海平面高度、冰川等),来评述我国区域气候未来变化的鼍级.从以上两个方面的情况看,我国区域的未来气候变化量级可能比现有模式预估的还要大.文章最后讨论了我国的气候变化脆弱区以及关键的气候变化要素问题.
從噹今國際上不同的氣候繫統模式模擬的全新世大暖期和末次盛冰期我國氣候變化量級和複原資料結果的對比,以及從目前氣候變化的趨勢(包括溫室氣體、氣溫、海洋溫度、海平麵高度、冰川等),來評述我國區域氣候未來變化的鼉級.從以上兩箇方麵的情況看,我國區域的未來氣候變化量級可能比現有模式預估的還要大.文章最後討論瞭我國的氣候變化脆弱區以及關鍵的氣候變化要素問題.
종당금국제상불동적기후계통모식모의적전신세대난기화말차성빙기아국기후변화량급화복원자료결과적대비,이급종목전기후변화적추세(포괄온실기체、기온、해양온도、해평면고도、빙천등),래평술아국구역기후미래변화적타급.종이상량개방면적정황간,아국구역적미래기후변화량급가능비현유모식예고적환요대.문장최후토론료아국적기후변화취약구이급관건적기후변화요소문제.
The Intergovernmental panel for Climate Change(IPCC) Report Series issued stronger and stronger conclusion that the climate change in the 20~(th) century is very much likely the largest climate change in recent 1000 years and warming the 20~(th) century is attributed to the green house gases increase. Recent studies suggest that the climate change is accelerated and the future climate change may well be larger than previously projected. However, there are opposite opinions as well both abroad and domestic. This article will discuss the issue of will the future climate change in China lager or smaller than projected. Our analyses will based on the climate model behavior in simulating the last glacial maximum and the mid-Holocene climates, as well as the recent changes in temperature, sea level, green house gases, mountain glaciers, and so on. All these information seems to lead to a conclusion that the future climate change in China might larger than projected by the state-of-the-art climate models. In order to better adjust to the climate change, recognizing the key vulnerable regions to climate change is essential. The paper suggests several key vulnerable regions, including the source region of the three major rivers (Yangtze River,Yellow River, and Lantsang River) ,the Central North China, North East China, North West China, and South Eastern China. Key issues for the source region of the three rivers include the fast melting of the mountain glaciers in the Tibetan Plateau region and the associated water cycle and supply to source region of the river. In the north part of the country, precipitation change and the related water resource change are the key concerns, particular for the Central North China. In the South Eastern China, we should pay more attention to the variation of climate extreme,including the flood,typhoon landfalling,and heat waves.