首页 | 官方网站   微博 | 高级检索  
     

藏北高原蒸发皿蒸发量及其影响因素的变化特征
引用本文:杜军,边多,鲍建华,拉巴,路红亚.藏北高原蒸发皿蒸发量及其影响因素的变化特征[J].水科学进展,2008,19(6):786-791.
作者姓名:杜军  边多  鲍建华  拉巴  路红亚
作者单位:1.西藏自治区气候中心, 西藏, 拉萨, 850001;
摘    要:采用气候倾向率方法,对藏北高原1971-2006年6个气象站年、季小型蒸发皿蒸发量及其影响气候因子的变化趋势进行了分析。结果表明:近36年藏北高原年蒸发皿蒸发量各站点均呈现显著的减少趋势,平均减少61.7mm/10a(通过99%显著性检验),以夏季减幅最明显。就地域分布而言,蒸发皿蒸发量的下降主要表现在藏北高原的中西部。蒸发量减少幅度随经度的增加减小,随海拔高度的升高而加大。影响蒸发皿蒸发量的主要气候因子日照时数、平均风速呈现显著下降趋势,平均相对湿度、降水量表现为显著增加,平均气温显著升高,平均最低气温的升温速率(0.54℃/10a)明显比平均最高气温的升温速率(0.17℃/10a)大,导致气温日较差的减小(-0.37℃/10a)。藏北高原平均气温日较差和日照时数的显著减小,以及平均相对湿度的明显增加可能是蒸发皿蒸发量显著下降的主要原因,降水量的增加和平均风速的明显减小在蒸发量减少趋势中的作用也不可忽视。

关 键 词:气候变化    蒸发皿蒸发量    影响因素    变化特征    藏北高原
收稿时间:2007-10-14

Changes of pan evaporations and its impact factors over northern Tibet in 1971-2006
DU Jun,BIAN Duo,BAO Jian-hua,LA Ba,LU Hong-ya.Changes of pan evaporations and its impact factors over northern Tibet in 1971-2006[J].Advances in Water Science,2008,19(6):786-791.
Authors:DU Jun  BIAN Duo  BAO Jian-hua  LA Ba  LU Hong-ya
Affiliation:1.The Climatic Center of Tibet, Lhasa 850001, China;2.Tibet Institute of Plateau Atmospheric and Environmental Science Research, Lhasa 850001, China;3.Meteorological Information and Network Center of Tibet, Lhasa 850001, China
Abstract:With the data of mthly 20cm pan evaporation and its impact climatic facts at 6 meteorological status over northern Tibet form 1971 to 2006, the trend is analyzed through the linear trend analysis.The main results are as follaus:(1) Significant negative trend of annual pan evaporation is detected at all stations of northern Tibet, and the mean rate of decrease is 6117 mm per 10-year (99% confidence level),especially in summer(-2018 mm per 10-year, 99% confidence level).The spatial distribution of the change rate shows that the decrease of annual pan evaporation mainly occurs in mid-western of northern Tibet, the decreasing rate declines with the increase of longitude and rises with the elevation of altitude.(2) Significant decrease trends of annual sunshine duration and wind speed are found over northern Tibet.Significant positive trends of annual mean relative humidity and precipitation are detected. So is significant increase trend of annual mean temperature, with its increase is 0.34 e per 10-year.While the increase trend of annual mean minimum temperature(0.54 e per 10-year) is bigger than that of annual mean maximum temperature(0.17 e per 10-year), and the trend of daily temperature range decrease significantly(-0.37 e per 10-year).And (3) it is thus obvious that the decrease of the pan evaporation is mainly caused by the significant decrease of the daily temperature range and sunshine duration as well as the obviously increase of the mean relative humidity.Precipitation and wind speed may also play an important role in the unknown mechanism.
Keywords:climatic change  pan evaporation  impact factors  change characteristic  northern Tibet
本文献已被 CNKI 维普 万方数据 等数据库收录!
点击此处可从《水科学进展》浏览原始摘要信息
点击此处可从《水科学进展》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司    京ICP备09084417号-23

京公网安备 11010802026262号