Boundary Layer Height's Variation Characteristics Research of Arid and Semiarid Areas over East Asia and North Africa in Recent 100 Years

  • ZHAO Yanru ,
  • ZHANG Kequan ,
  • MAO Wenqian ,
  • FAN Xu ,
  • LIU Chen ,
  • ZHANG Wenyu
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  • Key Laboratory for Semi-Arid Climate Change of the Ministry of Education, College of Atmospheric Sciences, Lanzhou University, Lanzhou 730000, China

Received date: 2016-06-17

  Online published: 2017-10-28

Abstract

Based on ERA-20C, ERA-Interim and ERA40, the ECMWF's reanalysis data, the interdecadal variation characteristics of the boundary-layer height of arid and semiarid areas over East Asia and North Africa spanning from 1900 to 2015 was analysed.The results showed that:(1) From 1900 to 2015, the average boundary layer of Arid and Semiarid Areas of East Asia and North Africa were 755 m and 834 m, respectively.It presented significant upward trend over East Asia with the climate tendency rate of 2.0 m·(10a)-1 and the decadal oscillation cycle of 20 years, and it presented downward trend over North Africa with the climate tendency rate of -0.6 m·(10a)-1 and the decadal oscillation cycle of 40 years.The year 1964 and 1940 were the significant turning point of East Asia and North Africa, respectively.After 1964, the boundary layer height of East Asia had a apparent rise and the boundary layer height's oscillation amplitude of North Africa increased obviously after 1940.(2) In arid and semiarid areas over East Asia, the most obvious upward trend region was at the east with the climate tendency rate of 10.7~12.4 m·(10a)-1, followed by central section, with the climate tendency rate of 3.8 m·(10a)-1, and the slowly upward trend region was at the north, with the climate tendency rate of 0.4~1.8 m·(10a)-1, the Taklamakan Desert showed downward trend with the climate tendency rate of -1.2 m·(10a)-1.Meanwhile, in the decadal fluctuations, the severe concussion presented in the sixties and seventies of East Asia boundary layer height was mainly associated with the change of central and east regions.(3) In arid and semiarid areas over North Africa, the central and north regions showed significant downward trend with the climate tendency rate of -5.1~-1.48 m·(10a)-1, and the south region showed upward trend with the climate tendency rate of 0.8~2.5 m·(10a)-1.However, in the decadal fluctuations, the intensified concussion after the forties of North Africa boundary layer height was mainly associated with the change of south region.

Cite this article

ZHAO Yanru , ZHANG Kequan , MAO Wenqian , FAN Xu , LIU Chen , ZHANG Wenyu . Boundary Layer Height's Variation Characteristics Research of Arid and Semiarid Areas over East Asia and North Africa in Recent 100 Years[J]. Plateau Meteorology, 2017 , 36(5) : 1304 -1314 . DOI: 10.7522/j.issn.1000-0534.2016.00107

References

[1]Arya S P S. 1981. Parameterizing the height of the stable atmospheric boundary layer[J]. J Appl Meteor, 20(10):1192-1202.
[2]Bachour D, Perez-Astudillo D. 2014. Boundary layer height measurements over Doha using Lidar[J]. Energy Procedia, 57:1086-1091.
[3]Bachtiar V S, Davies F, Danson F M. 2014. A combined model for improving estimation of atmospheric boundary layer height[J]. Atmos Environ, 98:461-473.
[4]Compton J C, Delgado R, Berkoff T A, et al. 2013. Determination of planetary boundary layer height on short spatial and temporal scales:A demonstration of the covariance wavelet transform in ground-based wind profiler and lidar measurements[J]. J Atmos Ocean Technol, 30(7):1566-1575.
[5]Coulter R L. 1979. A comparison of three methods for measuring mixing-layer height[J]. J Appl Meteor, 18(11):1495-1499.
[6]Couvreux F, Guichard F, Austin P H, et al. 2009. Nature of the mesoscale boundary layer height and water vapor variability observed 14 June 2002 during the IHOP_2002 campaign[J]. Mon Wea Rev, 137(1):414-432.
[7]Feng X, Wu B, Yan N. 2015. Amethod for deriving the boundary layer mixing height from MODIS atmospheric profile data[J]. Atmos, 6(9):1346-1361.
[8]He Q S, Mao J T, Chen J Y, et al. 2006. Observational and modeling studies of urban atmospheric boundary-layer height and its evolution mechanisms[J]. Atmos Environ, 40(6):1064-1077.
[9]Ma L M, Bao X W. 2016. Parametrization of planetary boundary-layer height with helicity and verification with tropical cyclone prediction[J]. Bound-Lay Meteor, 160:569-593.
[10]McGrath-Spangler E L. 2016. The impact of a boundary layer height formulation on the GEOS-5 model climate[J]. J Geophys Res:Atmos, 121(7):3263-3275.
[11]Molod A, Salmun H, Dempsey M. 2015. Estimating planetary boundary layer heights from NOAA profiler network wind profiler data[J]. J Atmos Ocean Technol, 32(9):1545-1561.
[12]Leventidou E, Zanis P, Balis D, et al. 2013. Factors affecting the comparisons of planetary boundary layer height retrievals from CALIPSO, ECMWF and radiosondes over Thessaloniki, Greece[J]. Atmos Environ, 74:360-366.
[13]Pal S, Xueref-Remy I, Ammoura L, et al. 2012. Spatio-temporal variability of the atmospheric boundary layer depth over the Paris agglomeration:An assessment of the impact of the urban heat island intensity[J]. Atmos Environ, 63:261-275.
[14]Patil M N, Patil S D, Waghmare R T, et al. 2013. Planetary boundary layer height over the Indian subcontinent during extreme monsoon years[J]. J Atmos Solar-Terrestrial Phys, 92:94-99.
[15]Randel W J, Wu F, Gaffen D J. 2000. Interannual variability of the tropical tropopause derived from radiosonde data and NCEP reanalyses[J]. J Geophys Res, 105(D12):15, 509-15, 523.
[16]Saeed U, Rocadenbosch F, Crewell S. 2015. Synergetic use of LiDAR and microwave radiometer observations for boundary-layer height detection[C]. Geoscience and Remote Sensing Symposium (IGARSS), 2015 IEEE International IEEE:3945-3948.
[17]Sausen R, Santer B D. 2003. Use of changes in tropopause height to detect human influences on climate[J]. Meteorologische Zeitschrift, 12(3):131-136.
[18]Sawyer V, Li Z. 2013. Detection, variations andintercomparison of the planetary boundary layer depth from radiosonde, lidar and infrared spectrometer[J]. Atmos Environ, 79:518-528.
[19]Schmid P, Niyogi D. 2012. A method for estimating planetary boundary layer heights and its application over the ARM Southern Great Plains Site[J]. J Atmos Ocean Technol, 29(3):316-322.
[20]Seidel D J, Ao C O, Li K. 2010. Estimating climatological planetary boundary layer heights from radiosonde observations:Comparison of methods and uncertainty analysis[J]. J Geophys Res:Atmos, 115(D16113). DOI:10. 1029/2009JD013680.
[21]Shrestha Sojan, Shrestha Saraswati, Maharjan Sangeeta, et al. 2015. Boundary layer characteristics over the central area of the Kathmandu Valley as revealed by sodar observation[J]. Journal of Institute of Science and Technology, 20(1):28-35.
[22]Stull R B. 1988. Anintroduction to boundary-layer meteorology[M]. Kluwer Academic Publishers, Norwell, MA:666.
[23]Von E A, Teixeira J. 2013. A planetary boundary layer height climatology derived from ECMWF reanalysis data[J]. J Climate, 26(17):6575-6590.
[24]Zhang Q, Zhang J, Qiao J, et al. 2012. Relationship of atmospheric boundary layer depth with thermodynamic processes at the land surface in arid regions of China[J]. Science China Earth Sciences, 54 (10):1585-1594.
[25]Zhang Y, Seidel D J, Zhang S. 2013. Trends in planetary boundary layer height over Europe[J]. J Climate, 26(24):10071-10076.
[26]Li Yanying, Qian Zheng'an, Xue Xinling, et al. 2009. Deep mixed layer in Northwest China dry area in summer half year and formation of the dry climate[J]. Plateau Meteor, 28(1):46-54.<br/>李岩瑛, 钱正安, 薛新玲, 等. 2009.西北干旱区夏半年深厚的混合层与干旱气候形成[J].高原气象, 28(1):46-54.
[27]Li Yanying, Zhang Qiang, Hu Xingcai, et al. 2012. Atmosphere boundary layer characteristics and their responses to wetness change over Arid Regions and Loess Plateau in Northwest China[J]. Journal of Glaciology and Geocryology, 34(5):1047-1058.<br/>李岩瑛, 张强, 胡兴才, 等. 2012.西北干旱区和黄土高原大气边界层特征对比及其对气候干湿变化的响应[J].冰川冻土, 34(5):1047-1058.
[28]Li Yanying, Zhang Qiang, Zhang Aiping, et al. 2016. Analysis on atmosphere boundary layer variation characteristics and their impact factors in arid region and semi-arid region over Northwest China[J]. Plateau Meteor, 35(2):385-396. DOI:10. 7522/j.issn. 1000-0534. 2014. 00153.<br/>李岩瑛, 张强, 张爱萍, 等. 2016.干旱半干旱区边界层变化特征及其影响因子分析[J].高原气象, 35(2):385-396.
[29]Liu Gang, Jiang Weimei, Luo Yunfeng. 2005. Status quo and prospects of researches on atmospheric boundary layer over inhomogeneous underlying surface[J]. Adv Earth Sci, 20(2):223-230.<br/>刘罡, 蒋维楣, 罗云峰. 2005.非均匀下垫面边界层研究现状与展望[J].地球科学进展, 20(2):223-230.
[30]Lü Daren, Chen Zeyu, Bian Jianchun, et al. 2008. Advances in researches on the characteristics of multi-scale processes of interactions between the stratosphere and the troposphere and its relations with weather and climate[J]. Chinese J Atmos Sci, 32(4):782-793.<br/>吕达仁, 陈泽宇, 卞建春, 等. 2008.平流层-对流层相互作用的多尺度过程特征及其与天气气候关系-研究进展[J].大气科学, 32(4):782-793.
[31]Qiao Juan. 2009. The temporal and spatial characteristics of atmospheric boundary layer and its formation mechanism over arid region of Northwest China[D]. Beijing:Chinese Academy of Meteorological Sciences.<br/>乔娟. 2009. 西北干旱区大气边界层时空变化特征及形成机理研究[D]. 北京: 中国气象科学研究院.
[32]Yang Yuhua, Liu Changhai, Jimy Dudhia, et al. 2016. Evaluation of two typical PBL parameterization schemes based on large-eddy simulation result[J]. Plateau Meteor, 35(1):172-180. DOI:10. 7522/j.issn. 1000-0534. 2014. 00138.<br/>杨玉华, 刘长海, Jimy D, 等. 2016.基于大涡模拟对两类典型边界层参数化方案的评估分析[J].高原气象, 35(1):172-180.
[33]Yue Ping, Niu Shengjie, Zhang Qiang, et al. 2008. An observation study of atmosphere boundary layer characteristic over semi-arid desert grassland in Mongolia Plateau on clear day in spring[J]. Plateau Meteor, 27(4):757-763.<br/>岳平, 牛生杰, 张强, 等. 2008.春季晴日蒙古高原半干旱荒漠草原地边界层结构的一次观测研究[J].高原气象, 27(4):757-763.
[34]Zhang Qiang, Hu Yinqiao, Zhao Ming. 1998. PBL characteristic simulation Under Desert-Oasis interaction[J]. Journal of Nanjing Institute of Meteorology, 20(1):104-113.<br/>张强, 胡隐樵, 赵鸣. 1998.绿洲与荒漠相互影响下大气边界层特征的模拟[J].南京气象学院学报, 20(1):104-113.
[35]Zhang Qiang, Hu Yinqiao. 2001. Scientific problems and advance of atmospherix boundary layer physics[J]. Adv Earth Sci, 16(4):526-532.<br/>张强, 胡隐樵. 2001.大气边界层物理学的研究进展和面临的科学问题[J].地球科学进展, 16(4):526-532.
[36]Zhang Qiang. 2003. Review of atmospheric boundary layer meterology[J]. Arid Meteor, 21(3):74-78.<br/>张强. 2003.大气边界层气象学研究综述[J].干旱气象, 21(3):74-78.
[37]Zhang Qiang, Wei Guo'an, Hou Ping. 2004. Observation studies of atmosphere boundary layer characteristic over Dunhuang Gobi in early summer[J]. Plateau Meteor, 23(5):587-597.<br/>张强, 卫国安, 侯平. 2004.初夏敦煌戈壁大气边界层结构特征的一次观测试[J].高原气象, 23(5):587-597.
[38]Zhang Qiang. 2007. Study on depth of atmospheric thermal boundary layer in Extreme Arid Desert Regions[J]. J Desert Res, 27(4):614-620.<br/>张强. 2007.极端干旱荒漠地区大气热力边界层厚度研究[J].中国沙漠, 27(4):614-620.
[39]Zhang Qiang, Zhao Yingdong, Wang Sheng, et al. 2007. A study on atmospheric thermal boundary layer structure in Extremely Arid Desert and Gobi Region on the clear day in summer[J]. Adv Earth Sci, 22(11):1150-1159.<br/>张强, 赵映东, 王胜, 等. 2007.极端干旱荒漠区典型晴天大气热力边界层结构分析[J].地球科学进展, 22(11):1150-1159.
[40]Zhang Qiang, Wang Sheng. 2008. A study on atmospheric boundary layer structure on a clear day in the Arid Region in Northwest China[J]. Acta Meteor Sinica, 66(4):599-608.<br/>张强, 王胜. 2008.典型干旱区晴天大气边界层结构及其陆面过程特征[J].气象学报, 66(4):599-608.
[41]Zhang Qiang, Wang Sheng, Zhang Jie, et al. 2009. The progresses on land surface processes and atmospheric boundary layer in Arid Regions[J]. Adv Earth Sci, 24(11):1185-1194.<br/>张强, 王胜, 张杰, 等. 2009.干旱区陆面过程和大气边界层研究进展[J].地球科学进展, 24(11):1185-1194.
[42]Zhao Cailing, Lü Shihua, Li Zhaoguo, et al. 2014. Numerical simulation of influence of land surface thermal condition on Badain Jaran Desert atmospheric boundary layer height in summer[J]. Plateau Meteor, 33(6):1526-1533. DOI:10. 7522/j.issn. 1000-0534. 2013. 00160.<br/>赵采玲, 吕世华, 李照国, 等. 2014.夏季巴丹吉林沙漠陆面热状况对边界层高度影响的模拟实验[J].高原气象, 33(6):1526-1533.
[43]Zhao Jianhua, Zhang Qiang, Wang Sheng, et al. 2013. Studies on frequency density of inversion intensity and height of atmospheric boundary layer in arid region of Northwest China[J]. Plateau Meteor, 32(2):377-386. DOI:10. 7522/j.issn. 1000-0534. 2012. 00038.<br/>赵建华, 张强, 王胜, 等. 2013.西北干旱区夏季大气边界层逆温强度和高度的频率密度研究[J].高原气象, 32(2):377-386.
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