Characteristics of Radiation Components in the Northern Margin of the Taklimakan Desert
Received date: 2012-09-25
Revised date: 2012-11-05
Online published: 2012-11-05
In this paper, the characteristics of radiation components are analyzed by using radiation observation data from Xiaotang meteorological station in the northern margin of the Taklimakan Desert. The results show that the monthly maximum component of shortwave radiation occurs in July, and maximum instantaneous global radiation (1 329.6 W\5m-2) emerges in June. Under the clear day conditions, seasonal variation of radiation components is very strong (weak) in summer (winter).The pattern of other radiation components take on inverse "U" shapes according to their diurnal changes except downwell long wave radiation. The daily total radiation of downwell long wave radiation under the floating dust and blowing dust condition is consistent that under the clear day condition. In addition, the maximum (minimum) daily total radiation of upwell long wave radiation occurs in clear day (cloudy day), and daily total radiation of upwell long wave radiation under the floating dust is between clear day and cloudy day. The surface albedo in winter is higher in Xiaotang area than in summer. The annual average surface albedo is 0.27 which is lower 10% than Taklimakan Desert hinterland, but higher far than oasis and plateau.
WANG Yan-hui1 , 2 , SHI Yu-guang3 , Mamtali\5Mamtimin1 , HE Qing1 , LI Shuai4 . Characteristics of Radiation Components in the Northern Margin of the Taklimakan Desert[J]. Journal of Desert Research, 2013 , 33(6) : 1824 -1831 . DOI: 10.7522/j.issn.1000-694X.2013.00242
[1]张强,曹晓彦.敦煌地区荒漠戈壁地表热量和辐射平衡特征的研究[J].大气科学,2003,27(2):245-254.
[2]杨兴国,马鹏里,王润元,等.陇中黄土高原夏季地表辐射特征分析[J].中国沙漠,2005,25(1):55-62.
[3]Monteith J L,Szeice G.The radiation balance of bare soil and vegetation[J]. Quarterly Journal of the Royal Meteorological Society,196l,87:159-170.
[4]Stanhil G.Radiation balance of natural and agricultural vegetation[J]. Quarterly Journal of the Royal Meteorological Society,1966,92:128-140.
[5]Moore C T.A comparative study of radiation balance above forest and grassland[J]. Quarterly Journal of the Royal Meteorological Society,1976,102:889-899.
[6]陈世强,吕世华,奥银焕,等.夏季不同天气背景条件下黑河中游不同下垫面的辐射特征[J].中国沙漠,2008,28(3):514-518.
[7]张凯,王润元,张强,等.绿洲荒漠过渡带夏季晴天地表辐射和能量平衡及小气候特征[J].中国沙漠,2007,27(6):1055-1061.
[8]邹基玲,季国良,侯旭宏.张掖地区春小麦生长期的辐射平衡观测[J].高原气象,1994,13(3):353-358.
[9]陈渭民,洪刚.由GMS卫星资料获取我国夏季地表辐射收支[J].大气科学,1997,21(2):238-246.
[10]李江风.塔克拉玛干沙漠和周边山区天气气候[M].北京:科学出版社,2003.
[11]卞林根,陆龙骅,逯昌贵,等.1998年夏季青藏高原辐射平衡分量特征[J].大气科学,2001,25(5):577-588.
[12]季国良,侯旭宏,吕兰芝,等.干旱地区不同下垫面的辐射收支[J].太阳能学报,2004,25(1):37-40.
[13]王胜,张强,卫国安.敦煌绿洲-戈壁过渡带地表辐射与能量特征分析[J].高原气象,2005,24(4):556-562.
[14]陈世强,文莉娟,吕世华,等.JTEX不同下垫面的辐射特征对比分析[J].太阳能学报,2006,7(7):713-718.
[15]孙昭萱,张强.黄土高原半干旱区陆面温度和能量的气候特征分析[J].中国沙漠,2011,31(5):1302-1308.
[16]顾润源,武荣盛,周伟灿,等.内蒙古半干旱草原沙尘天气对近地层微气象学特征影响分析[J].中国沙漠,2012,32(3):815-823.
[17]李帅,胡列群,何清,等.塔克拉玛干沙漠腹地地表辐射收支特征研究[J].中国沙漠,2012,32(4):1035-1044.
[18]张瑞军,何清,孔丹,等.塔克拉玛干沙漠北缘沙尘暴源区地表沉积物粒度特征[J].干旱区研究,2008,25(6):887-893.
[19]何清,缪启龙,张瑞军,等.塔克拉玛干沙漠肖塘地区空气动力学粗糙度分析[J].中国沙漠,2008,28(6):1011-1016.
[20]阴俊,谈建国.上海地区地面太阳紫外辐射的观测和分析[J].热带气象学报,2006,22(1):86-90.
[21]季国良.1982年8月-1983年7月青藏高原地区的辐射与气候[J].高原气象,1985,4(S2):10-20.
[22]何清.塔克拉玛干沙漠中大气边界层结构及地-气相互作用观测研究[D].南京:南京信息工程大学,2009.
[23]邹基玲,候旭宏,季国良.黑河地区夏末太阳辐射特征的初步分析[J].高原气象,1992,11(4):381-388.
[24]周允华,陆魁东.冬小麦田净余辐射与总辐射的关系[M]//牛文元,周允华,张翼.农田生态系统能量物质交换.北京:气象出版社,1987:25-35.
[25]Agnstrom A. Solar and terrestrial radiation[J].Quarterly Journal of the Royal Meteorological Society,1924,52(8):397.
/
〈 |
|
〉 |