CAJ | 학술논문

在利用 MODIS 卫星的云产品资料对 CFSR（Climate Forecast System Reanalysis）再分析资料云产品质量进行检验评估的基础上，采用 CFSR 资料对1979-2009年全球总云量及低、中、高云量的平均分布及其随纬度的变化进行了分析；用经验模态分解（EMD）方法分析了近30年全球云量的变化趋势，结果表明：（1）全球近30年平均总云量约为59％，全球总云量及低云量、中云量都有明显的纬向分布特征，全球总云量有3个峰值带和3个低值带。（2）低云量的海陆分布差异较明显，陆地上的低云量明显低于海洋上的，除了两个极圈附近，南半球各纬度的低云量都比北半球相应纬度上的都要多；高云量的高值、低值中心均集中在赤道附近到南、北半球30°之间的中低纬度，并且低值中心主要分布在大洋的东部。（3）总云量的总变化趋势为增长，具体表现为随时间呈现先略减少后大幅增加趋势，其突变点大致在1993年，在1993年之后，总云量显著增多。低云量和高云量均呈现增长趋势，中云量则相反，呈减少趋势。低云量增幅最明显，接近2％，中、高云量则增减幅度较小。
재이용 MODIS 위성적운산품자료대 CFSR（Climate Forecast System Reanalysis）재분석자료운산품질량진행검험평고적기출상，채용 CFSR 자료대1979-2009년전구총운량급저、중、고운량적평균분포급기수위도적변화진행료분석；용경험모태분해（EMD）방법분석료근30년전구운량적변화추세，결과표명：（1）전구근30년평균총운량약위59％，전구총운량급저운량、중운량도유명현적위향분포특정，전구총운량유3개봉치대화3개저치대。（2）저운량적해륙분포차이교명현，륙지상적저운량명현저우해양상적，제료량개겁권부근，남반구각위도적저운량도비북반구상응위도상적도요다；고운량적고치、저치중심균집중재적도부근도남、북반구30°지간적중저위도，병차저치중심주요분포재대양적동부。（3）총운량적총변화추세위증장，구체표현위수시간정현선략감소후대폭증가추세，기돌변점대치재1993년，재1993년지후，총운량현저증다。저운량화고운량균정현증장추세，중운량칙상반，정감소추세。저운량증폭최명현，접근2％，중、고운량칙증감폭도교소。
Based on the verification and evaluation of the quality of CFSR (Climate Forecast System Reanal-ysis)cloud amount reanalysis data by satellite remote sensing data MODIS,we analyze the average distri-bution of global total and low,middle,high cloud amount from 1979 to 2009 as well as the cloud amount variation along the latitude.Also,by using empirical mode decomposition (EMD)method,we analyze the change trend of each cloud amount in the recent 30 years.The results show that:(1 )the global average total cloud amount in recent 30 years is about 59%,the global total and low,middle,high cloud amounts have obvious zonal distribution characteristics,and there are 3 peak value zones and 3 low value zones for the total cloud amount.(2)The difference of land-sea distribution for low cloud amount is obvious and the amount of low cloud over the land is significantly lower than that over the ocean.Except for the two polar regions,the amount of low cloud in the Southern Hemisphere is more than that of the corresponding lati-tudes in the Northern Hemisphere;the locations of maximum and minimum of high cloud amount are be-tween the mid-low latitudes (30°)of Southern,and Northern Hemispheres respectively.In addition,the low value center mainly distributes in the eastern ocean.(3)The variation of total cloud amount is in an increasing trend,and it is specificly displayed as skyrocketed after a slightly decrease with the time.Its jump point year is around 1993,after which total cloud amount increases significantly.Low and high cloud amounts show a decreasing trend,in contrast,middle cloud amount is decreasing.Low cloud amount in-creases the most by nearly 2% while the change of high cloud amount is smaller.