Study on Variation of Snow Cover and Its Orographic Impact over Qinghai-Xizang Plateau during 2001-2012

  • GUO Jianping ,
  • LIU Huan ,
  • AN Linchang ,
  • WANG Pengxiang ,
  • GAO Mei
Expand
  • State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081, China;2. Natioanl Meteorological Center, China Meteorological Administration, Beijing 100081, China;3. Tibet Autonomous Region Meteorological Bureau, Lhasa 850001, China

Received date: 2013-11-20

  Online published: 2016-02-28

Abstract

The snow cover fraction(SCF) data during the period 2001 through 2012 from MODIS aboard Terra of NASA are used to derive the spatio-temporal distribution of snow,and to calculate its variation trend over the Qinghai-Xizang Plateau(QXP) using statistic analysis methods.The SCF during the months from October through the following April dominates compared with other months.Persistent snow area reaches the maximum of 92.93×104 km2 in February.It begins to decrease gradually as of May,hits to the bottom line of 12.37×104 km2 in July.Beginning in September,SCF goes up sharply,leveling off in October.Overall,the annual mean snow area over the QXP oscillates between 55×104~80×104 km2,showing a three-year variation cycle.Also,altitude is found to be able to exert significant influence on SCF.The higher the altitude is,the higher the SCF is over most parts of the QXP except over southwest QXP.For regions below 5 km,there is a monotonic seasonal variation trend,i.e.,higher winter SCF and lower summer SCF.In contrast,for regions above 5 km,there is a bi-modal variation trend.Aspect derived from digital elevation model can exert great influence on SCF as well.Northerly aspect corresponds to the maximum SCF,followed by westerly and easterly,and then southerly aspects.This is likely due to the solar radiation difference caused by various aspects.Similarly,SCF increases rapidly with slope during October to the following April,and then almost stays invariant during May through September.

Cite this article

GUO Jianping , LIU Huan , AN Linchang , WANG Pengxiang , GAO Mei . Study on Variation of Snow Cover and Its Orographic Impact over Qinghai-Xizang Plateau during 2001-2012[J]. Plateau Meteorology, 2016 , 35(1) : 24 -33 . DOI: 10.7522/j.issn.1000-0534.2014.00140

References

[1]Chang A T C,Foster J L,Hall D K.1987.Nimbus-7 SMMR derived global snow cover parameters[J].Annals of Glaciology,9(9):39-44.
[2]Che T,Xin L,Jin R,et al.2008.Snow depth derived from passive microwave remote-sensing data in China[J].Annals of Glaciology,49(1):145-154.
[3]Cohen J,Rind D.1991.The effect of snow cover on the climate[J].J Climate,4(7):689-706.
[4]Dahe Q,Shiyin L,Peiji L.2006.Snow cover distribution,variability,and response to climate change in western China[J].J Climate,19(9):1820-1833.
[5]Frei A,Robinson D A.1999.Northern Hemisphere snow extent:Regional variability 1972-1994[J].Int J Climatol,19(14):1535-1560.
[6]Hall D K,Foster J L,Salomonson V V,et al.2001.Development of a technique to assess snow-cover mapping errors from space[J].IEEE Trans Geosci Remote Sens,39(2):432-438.
[7]Hall D K,Kelly R E J,Riggs G A,et al.2002.Assessment of the relative accuracy of hemispheric-scale snow-cover maps[J].Annals of Glaciology,34(1):24-30.
[8]Moore G W K.2004.Mount everest snow plume:A case study[J].Geophy Res Lett,31(22):L22102.DOI:10.1029/2004GL021046.
[9]Pu Z,Xu L,Salomonson V V.2007.MODIS/Terra observed seasonal variations of snow cover over the Tibetan Plateau[J].Geophy Res Lett,34(6):L06706.DOI:10.1029/2007GL029262.
[10]Riggs G A,Hall D K,Salomonson V V.2006.MODIS snow products user guide to collection 5[J/OL].http://modis-snow-ice.gsfc.nasa.gov/sugkc2.html 80.
[11]Robinson D A,Keimig F T,Dewey K F.1991.Recent variations in Northern Hemisphere snow cover[C].Proc.15th Annual Climate Diagnostics Workshop,219-224.
[12]Walland D J,Simmonds I.1996.Modelled atmospheric response to changes in Northern Hemisphere snow cover[J].Climate Dyn,13(1):25-34.
[13]Wu T W,Qian Z A.2003.The relation between the Tibetan winter snow and the Asian summer monsoon and rainfall:An observational investigation[J].J Climate,16(12):2038-2051.
[14]Yanai M,Li C,Song Z.1992.Seasonal heating of the Tibetan Plateau and its effects on the evolution of the Asian summer monsoon[J].J Meteor Soc Japan,70(1B):319-351.
[15]Yang S.1996.ENSO-snow-monsoon associations and seasonal-interannual predictions[J].Int J Climatol,16(2):125-134.
[16]车涛,李新,高峰.2004.青藏高原积雪深度和雪水当量的被动微波遥感反演[J].冰川冻土,26(3):363-368.Che Tao,Li Xin,Gao Feng.2004.Estimation of snow water equivalent in the Tibetan Plateau using passive microwave remote sensing data(SSM/I)[J].J Glaciology Geocryology,26(3):363-368.
[17]陈爱军,王飞,卞林根,等.2012.青藏高原地区 MODIS 反照率两种反演结果差异的对比分析[J].高原气象,31(6):1479-1487.Chen Aijun,Wang Fei,Bian Lingen,et al.2012.Study on difference between two kinds of MODIS albedo over the Qinghai-Xizang Plateau[J].Plateau Meteor,31(6):1479-1487.
[18]除多,姬秋梅,普次.2007.利用 EOS/MODIS 数据估算西藏藏北高原地表草地生物量[J].气象学报,65(4):612-621.Chu Duo,Ji Qiumei,Pu Ci.2007.Estimating grassland biomass in north Tibetan Plateau using EOS/MODIS[J].Acta Meteor Sinica,65(4):612-621.
[19]除多,拉巴卓玛,拉巴,等.2011.珠峰地区积雪变化与气候变化的关系[J].高原气象,30(3):576-582.Chu Duo,Laba Zhuoma,La Ba,et al.2011.Link between perennial snow cover variations and climate change in Qomolangma nature preserve from 1975 to 2000[J].Plateau Meteor,30(3):576-582.
[20]郭艳君,翟盘茂,李威.2004.NOAA 卫星遥感与常规观测中国积雪的对比研究[J].冰川冻土,26(6):755-760.Guo Yanjun,Zhai Panmao,Li Wei.2004.Snow cover in China,derived from NOAA satellite remotesensing and conventional observation[J].J Glaciology Geocryology,26(6):755-760.
[21]过霁冰,徐祥德,施晓晖,等.2012.青藏高原冬季积雪关键区视热源特征与中国西南春旱的联系[J].高原气象,31(4):900-909.Guo JiBing,Xu XiangDe,Shi XiaoHui,et al.2012.Characteristics of winter apparent heat source in the key area of snow cover on Qinghai-Xizang Plateau and spring drought in southwest China[J].Plateau Meteor,31(4):900-909.
[22]李川,张廷军,陈静.2004.近 40年青藏高原地区的气候变化-NCEP 和 ECMWF 地面气温及降水再分析和实测资料对比分析[J].高原气象,23(增刊1):97-103.Li Chuan,Zhang Tinjun,Chen Jing.2004.Climatic change of Qinghai-Xizang Plateau region in recent 40-year reanalysis and surface observation data-contrast of observational data and NCEP,ECMWF surface air temperature and precipitation[J].Plateau Meteor,23(supp1):97-103.
[23]李跃清.2002.近40年青藏高原东侧地区云,日照,温度及日较差的分析[J].高原气象,21(3):327-332.Li Yueqing.2002.Analyses of cloudiness,sunshine,temperature and daily range on the eastern side of Qinghai-Xizang Plateau in recent 40 years[J].Plateau Meteor,21(3):327-332.
[24]刘健.2013.利用卫星数据分析青藏高原云微物理特性[J].高原气象,32(1):38-45.Liu Jian.2013.Analysis on cloud microphysical property over Qinghai-Xizang Plateau using satellite data[J].Plateau Meteor,32(1):38-45.DOI:10.7522/j.issn.1000-0534.2013.00005.
[25]马林,李锡福,张青梅,等.2001.青藏高原东部牧区冬季雪灾天气的形成及其预报[J].高原气象,20(3):325-331.Ma Lin,Li Xifu,Zhang Qingmei,et al.2001.The forming and forecasting of winter snow-disaster weather in easten pastoral-area of Qinghai-Xizang Plateau[J].Plateau Meteor,20(3):325-331.
[26]唐红玉,李锡福,李栋梁.2014.青藏高原春季积雪多、少年中低层环流对比分析[J].高原气象,33(5):1190-1196,Tang Hongyu,Li Xifu,Li Dongliang.2014.Contrast of circulation pattern related to more and less spring snow cover over Qinghai-Xizang Plateau[J].Plateau Meteor,33(5):1190-1196.DOI:10.7522/j.issn.1000-0534.2013.00125.
[27]王叶堂,何勇,侯书贵.2007.2000-2005年青藏高原积雪时空变化分析[J].冰川冻土,29(6):855-861.Wang Yetang,He Yong,Hou Shugui.2007.Analysis of the temporal and spatial variations of snow cover over the Tibetan Plateau based on MODIS[J].J Glaciology Geocryology,29(6):855-861.
[28]韦志刚,黄荣辉,陈文,等.2002.青藏高原地面站积雪的空间分布和年代际变化特征[J].大气科学,26(4):496-508.Wei Zhigang,Huang Ronghui,Chen Wen,et al.2002.SPatial distribution sand interdecadal variations of the snow at the Tibetan Plateau weather stations[J].Chinese J Atmos Sci,26(4):496-508.
[29]韦志刚,黄荣辉,董文杰.2003.青藏高原气温和降水的年际和年代际变化[J].大气科学,27(2):157-170.Wei Zhigang,Huang Ronghui,Dong Wenjie.2003.Interannual and interdecadal variations of air temperature and precipitation over the Tibetan Plateau[J].Chinese J Atmos Sci,27(2):157-170.
[30]文军,Dai M,Deroin J P,等.2006.利用MODIS和ASAR资料估算青藏高原念青唐古拉山脉地区冰雪范围及厚度[J].冰川冻土,28(1):54-61.Wen Jun,Dai M,Deroin J P,et al.2006.Extent and depth of snow cover over the nyainqêntanghla range derived from ASAR and MODIS data[J].J Glaciology Geocryology,28(1):54-61.
[31]许立言,武炳义.2012.欧亚大陆积雪与2010年中国春末夏初降水的关系[J].高原气象,31(3):706-714.Xu Liyan,Wu Bingyi.2012.Relationship between Eurasian snow cover and late-spring and early-summer rainfall in China in 2010[J].Plateau Meteor,31(3):706-714.
[32]叶笃正.1979.青藏高原气象学[M].北京.科学出版社,300.Ye Duzheng.1979.Qinghai-Xizang Plateau meteorology[M].Beijing:Science Press,300.
[33]于琳琳,陈海山.2012.青藏高原4月陆面状况和地表加热异常与中国夏季降水的联系[J].高原气象,31(5):1173-1182.Yu Linlin,Chen Haishan.2012.Possible linkages among anomalous land surface condition,surface heating in Qinghai-Xizang Plateau in april and summer precipitation in China[J].Plateau Meteor,31(5):1173-1182.
[34]张镱锂,李炳元,郑度.2002.论青藏高原范围与面积[J].地理研究,21(1):1-8.Zhang Yili,Li Bingyuan,Zheng Du.A discussion on the boundary and area of the Tibetan Plateau in China[J].Geograph Res,21(1):1-8.
[35]朱玉祥,丁一汇,刘海文.2009.青藏高原冬季积雪影响我国夏季降水的模拟研究[J].大气科学,33(5):903-915.Zhu Yuxiang,Ding Yihui,Liu Haiwen.2009.Simulation of the influence of winter snow depth over the Tibetan Plateau on summer rainfall in China[J].Chinese J Atmos Sci,33(5):903-915.
[36]朱玉祥,丁一汇.2007.青藏高原积雪对气候影响的研究进展和问题[J].气象科技,35(1):1-8.Zhu Yuxiang,Ding Yihui.2007.Influences of snow cover over Tibetan Plateau on weather and climate:Advances and problems[J].Meteor Sci Tech,35(1):1-8.
[37]卓嘎,边巴次仁,杨秀海,等.2013.近30年西藏地区大气可降水量的时空变化特征[J].高原气象,32(1):23-30.Zhuo Ga,Bianba Ciren,Yang Xiuhai,et al.2013.Spatial and temporal changes of atmospheric precipitable water in Tibetan region in recent 30 years[J].Plateau Meteor,32(1):23-30.DOI:10.7522/j.issn.1000-0534.2013.00003.
Outlines

/