气候变化研究进展
氣候變化研究進展
기후변화연구진전
ADVANCES IN CLIMATE CHANGE RESEARCH
2010年
2期
113-118
,共6页
气候变化%干湿气候%因子分析%干季%云南
氣候變化%榦濕氣候%因子分析%榦季%雲南
기후변화%간습기후%인자분석%간계%운남
climate change%dry-wet climate%factor analysis%dry season%Yunnan
从影响自然干湿变化的多种因素出发,基于云南省15个站点1961-2007年干季9项气候要素实测数据,应用因子分析法研究云南干季干湿气候变化特征.提取了表征干季干湿气候变化的3个公共因子,阐明了云南干季干湿气候变化特点和原因.结果显示:1960年代以来5个年代干湿气候变化明显,变化原因各异,总变化趋势是湿度缓降、干旱强度渐强,1960-1980年代都处于中等干旱偏弱态势,进入1990年代后降水时间分布不均和气候变暖导致干季气候持续典型偏干,干季总降水量变化趋势有不确定性,年代际变化明显、变率不大,但其年际变化突出造成干季干湿状况年际波动大.
從影響自然榦濕變化的多種因素齣髮,基于雲南省15箇站點1961-2007年榦季9項氣候要素實測數據,應用因子分析法研究雲南榦季榦濕氣候變化特徵.提取瞭錶徵榦季榦濕氣候變化的3箇公共因子,闡明瞭雲南榦季榦濕氣候變化特點和原因.結果顯示:1960年代以來5箇年代榦濕氣候變化明顯,變化原因各異,總變化趨勢是濕度緩降、榦旱彊度漸彊,1960-1980年代都處于中等榦旱偏弱態勢,進入1990年代後降水時間分佈不均和氣候變暖導緻榦季氣候持續典型偏榦,榦季總降水量變化趨勢有不確定性,年代際變化明顯、變率不大,但其年際變化突齣造成榦季榦濕狀況年際波動大.
종영향자연간습변화적다충인소출발,기우운남성15개참점1961-2007년간계9항기후요소실측수거,응용인자분석법연구운남간계간습기후변화특정.제취료표정간계간습기후변화적3개공공인자,천명료운남간계간습기후변화특점화원인.결과현시:1960년대이래5개년대간습기후변화명현,변화원인각이,총변화추세시습도완강、간한강도점강,1960-1980년대도처우중등간한편약태세,진입1990년대후강수시간분포불균화기후변난도치간계기후지속전형편간,간계총강수량변화추세유불학정성,년대제변화명현、변솔불대,단기년제변화돌출조성간계간습상황년제파동대.
From the angle of manifold factors affecting natural dry-wet change, the research was performed in order to further understand and deal with climate change scientifically. Based on 1961-2007 observed data of nine climatic elements from 15 stations, the factor analysis was used to investigate the dry-wet climate change in the dry season in Yunnan. Three common factors were extracted from the nine climate variables to describe the dry-wet climate change for the dry season; and the features and causes of the change were clarified. The results show that the dry-wet climate has evidently changed since the early 1960s because of the influences of different factors in different decades. The general trends of dry-wet climate change were described as slow decrease in humidity and gradual enhancement in drought intensity. The climates were in a state of the drought of a weaker medium strength during the 1960s-1980s; but since the early 1990s, the markedly drier climate has continually occurred in the dry season owing to the misproportionally temporal distribution of rainfall and the climate wanning. The variation tendency of the total precipitation for the dry season had uncertainty regardless of its obvious interdecadal changes of relatively small variance ratio; and its prominent interannual change led to the big interannnal fluctuations for dry-wet climate.