摘要
利用20个气象站1960-2006年的逐日气象资料,采用FAOPenman-Monteith模型,计算出祁连山及河西走廊各气象站的月潜在蒸发量,在此基础上计算各气象站的月湿润指数,然后进行季节、年地表湿润指数的统计,进而对研究区地表干湿状况的时空变化进行分析.结果表明:祁连山及河西走廊在20世纪80年代之前地表相对干旱,之后相对湿润,自60年代以来地表湿润指数有逐年增大的趋势;年地表湿润指数的年际变化率为0.0014a-1,相关系数为0.4281,通过了0.01的置信度检验,表明地表湿润状况有明显改善,其中春季和冬季增加趋势明显,夏季增加趋势和秋季减小趋势不太明显.地表干湿变化趋势在空间上有差异,东部表现为东西差异,自东向西逐渐变湿,乌鞘岭以东呈变干趋势,其他大部分地区显著变湿,中部大部分地区呈不明显的变干趋势,而托来南山以北地区显著变干,张掖绿洲显著变湿,西部除敦煌以西呈不显著的变湿趋势,其他大部分地区显著变湿.
Based on the climatic data of 20 weather stations from 1960 to 2006,the monthly potential evaporation was calculated using the Penman-Monteith model,and then the monthly humid index was reconstructed in Qilian Mountains and Hexi Corridor.In order to study the temporal and spatial characteristics of the dry-wet conditions in the study area,the seasonal and annual humid indices were analyzed.Statistical results indicate that the study area was drier before 1980s,and the humid index has been on the rise since 1960s.The change rate of annual humid index was 0.001 4 a-1,which indicates that the humid condition of study area has become better obviously,especially in spring and winter.The spatial change of dry-wet conditions of the study area shows that it is becoming wetter from eastern to western parts in east region with an exception of the eastern area of Wushaoling Mountains which is becoming drier;for most middle region,it is also becoming drier insignificantly except for the northern area of Shule South Mountains and Zhangye oasis,and,it is becoming wetter in most western region except for the western area of Dunhuang City where it is becoming wetter insignificantly.
出处
《地球科学（中国地质大学学报）》
EI
CAS
CSCD
北大核心
2010年第2期268-276,共9页
Earth Science-Journal of China University of Geosciences
基金
国家重点基础研究发展"973"计划(No.2007CB411201)
国家自然科学基金项目(No.40971019)
中国科学院"西部之光"人才培养计划"西部博士资助项目"(No.O828A11001)
西北师范大学青年教师基金(No.NWNU-LKQN-08-03)
西北师范大学自然地理学省级重点学科资助
关键词
湿润指数
年代际变化
年际变化
祁连山
河西走廊
水文地质学
humid index
interdecadal variation
interannua variation
Qilian Mountains
Hexi Corridor
hydrogeology.
