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Summer atmospheric boundary layer structure in the hinterland of Taklimakan Desert, China

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Abstract

Understanding the characteristics of the structure of desert atmospheric boundary layer and its land surface process is of great importance to the simulations of regional weather and climate. To investigate the atmospheric boundary layer structure and its forming mechanism of Taklimakan Desert, and to improve the accuracy and precision of regional weather and climate simulations, we carried out a GPS radiosonde observation experiment in the hinterland of Taklimakan Desert from 25 June to 3 July, 2015. Utilizing the densely observed sounding data, we analyzed the vertical structures of daytime convective boundary layer and nighttime stable boundary layer in summer over this region, and also discussed the impacts of sand-dust and precipitation events on the desert atmospheric boundary layer structure. In summer, the convective boundary layer in the hinterland of Taklimakan Desert developed profoundly and its maximum height could achieve 4,000 m; the stable boundary layer at nighttime was about 400–800-m thick and the residual mixing layer above it could achieve a thickness over 3,000 m. Sand-dust weather would damage the structures of nighttime stable boundary layer and daytime convective boundary layer, and the dust particle swarm can weak the solar radiation absorbed by the ground surface and further restrain the strong development of convective boundary layer in the daytime. Severe convective precipitation process can change the heat from the ground surface to the atmosphere in a very short time, and similarly can damage the structure of desert atmospheric boundary layer remarkably. Moreover, the height of atmospheric boundary layer was very low when raining. Our study verified the phenomenon that the atmospheric boundary layer with supernormal thickness exists over Taklimakan Desert in summer, which could provide a reference and scientific bases for the regional numerical models to better represent the desert atmospheric boundary layer structure.

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References

  • Angevine W M, White A B, Avery S K. 1994. Boundary-layer depth and entrainment zone characterization with a boundary-layer profiler. Boundary-Layer Meteorology, 68(4): 375–385.

    Article  Google Scholar 

  • Charney J G. 1975. Dynamics of deserts and drought in the Sahel. Quarterly Journal of the Royal Meteorological Society, 101(428): 193–202.

    Article  Google Scholar 

  • Cuesta J, Edouart D, Mimouni M, et al. 2008. Multiplatform observations of the seasonal evolution of the Saharan atmospheric boundary layer in Tamanrasset, Algeria, in the framework of the African Monsoon Multidisciplinary Analysis field campaign conducted in 2006. Journal of Geophysical Research: Atmospheres, 113(D23): D00C07.

    Google Scholar 

  • Cunnington W M, Rowntree P R. 1986. Simulations of the Saharan atmosphere-dependence on moisture and albedo. Quarterly Journal of the Royal Meteorological Society, 112(474): 971–999.

    Google Scholar 

  • Deardorff J W. 1970. Convective velocity and temperature scale for the unstable planetary boundary layer and for Rayleigh convection. Journal of the Atmospheric Sciences, 27(8): 1211–1213.

    Article  Google Scholar 

  • Gamo M. 1996. Thickness of the dry convection and large-scale subsidence above deserts. Boundary-Layer Meteorology, 79(3): 265–278.

    Article  Google Scholar 

  • Garratt J R. 1992. The Atmospheric Boundary Layer. Cambridge: Cambridge University Press, 1–3.

    Google Scholar 

  • Garratt J R. 1993. Sensitivity of climate simulations to land-surface and atmospheric boundary-layer treatments-a review. Journal of Climate, 6(3): 419–448.

    Article  Google Scholar 

  • Gornitz V, Nasa. 1985. A survey of anthropogenic vegetation changes in West Africa during the last century-climatic implications. Climatic Change, 7(3): 285–325.

    Article  Google Scholar 

  • He Q. 2009. Observation study of atmospheric boundary layer structure and land atmosphere interaction in the Tazhong of Taklimakan Desert. PhD Dissertation. Nanjing: Nanjing University of Information Science & Technology, 80–100. (in Chinese)

    Google Scholar 

  • He Q, Jing L L, Yang X H, et al. 2010a. Analysis on O3 concentration and affecting factors for boundary-layer in hinterland of Taklimakan Desert in Autumn. Plateau Meteorology, 29(1): 214–221. (in Chinese)

    Google Scholar 

  • He Q, Liu Q, Yang X H, et al. 2010b. Profiles of atmosphere boundary layer Ozone in winter over hinterland of Taklimakan Desert. Journal of Desert Research, 30(4): 909–916. (in Chinese)

    Google Scholar 

  • Henderson-Sellers A. 1980. Albedo changes-surface surveillance from satellites. Climatic Change, 2(3): 275–281.

    Article  Google Scholar 

  • Hu Y Q, Gao Y X. 1994. Some new understandings of processes at the land surface in arid area from the HEIFE. Acta Meteorologica Sinica, 52(3): 285–296. (in Chinese)

    Google Scholar 

  • Huang Q, Marsham J H, Parker D J, et al. 2010. Simulations of the effects of surface heat flux anomalies on stratification, convective growth, and vertical transport within the Saharan boundary layer. Journal of Geophysical Research: Atmospheres, 115(D5), doi: 10.1029/2009JD012689.

    Google Scholar 

  • Hyun Y K, Kim K E, Ha K J. 2005. A comparison of methods to estimate the height of stable boundary layer over a temperate grassland. Agricultural and Forest Meteorology, 132(1–2): 132–142.

    Article  Google Scholar 

  • Lare A R, Nicholson S E. 1990. A climatonomic description of the surface energy balance in the central Sahel. Part I: shortwave radiation. Journal of Applied Meteorology, 29(2): 123–137.

    Google Scholar 

  • Li J G, Ao Y H, Li Z G, et al. 2014. Characteristics of atmospheric boundary layer over the Badain Jaran desert in summer. Journal of Desert Research, 34(2): 488–497. (in Chinese)

    Google Scholar 

  • Liu Y Q, He Q, Zhang H S, et al. 2012. Improving the CoLM in Taklimakan Desert hinterland with accurate key parameters and an appropriate parameterization scheme. Advances in Atmospheric Sciences, 29(2): 381–390.

    Article  Google Scholar 

  • Marsham J H, Parker D J, Grams C M, et al. 2008. Observations of mesoscale and boundary-layer scale circulations affecting dust transport and uplift over the Sahara. Atmospheric Chemistry and Physics, 8(23): 6979–6993.

    Article  Google Scholar 

  • Messager C, Parker D J, Reitebuch O, et al. 2010. Structure and dynamics of the Saharan atmospheric boundary layer during the West African monsoon onset: observations and analyses from the research flights of 14 and 17 July 2006. Quarterly Journal of the Royal Meteorological Society, 136(S1): 107–124.

    Article  Google Scholar 

  • Qiao J. 2009. The temporal and spatial characteristics of atmospheric boundary layer and its formation mechanism over arid region of northwest China. MSc Thesis. Beijing: Chinese Academy of Meteorological Sciences, 6–12. (in Chinese)

    Google Scholar 

  • Redelsperger J L, Guichard F, Mondon S. 2000. A parameterization of mesoscale enhancement of surface fluxes for large-scale models. Journal of Climate, 13(2): 402–421.

    Article  Google Scholar 

  • Seibert P, Beyrich F, Gryning S E, et al. 2000. Review and intercomparison of operational methods for the determination of the mixing height. Atmospheric Environment, 34(7): 1001–1027.

    Article  Google Scholar 

  • Sivakumar M V K. 2007. Interactions between climate and desertification. Agricultural and Forest Meteorology, 142(2–4): 143–155.

    Article  Google Scholar 

  • Stull R B. 1988. An Introduction to Boundary Layer Meteorology. Dordrecht: Kluwer Academic Publisher, 649.

    Book  Google Scholar 

  • Su C X, Hu Y Q. 1987. The structure of the oasis cold island in the planetary boundary layer. Acta Meteorologica Sinica, 45(3): 322–328. (in Chinese)

    Google Scholar 

  • Takemi T. 1999. Structure and evolution of a severe squall line over the arid region in northwest China. Monthly Weather Review, 127(6): 1301–1309.

    Article  Google Scholar 

  • Wang M Z, Wei W S, He Q, et al. 2012. Radar wind profiler observations of convective boundary layer during clear-air days over Taklimakan desert. Meteorological Monthly, 38(5): 577–584. (in Chinese)

    Google Scholar 

  • Wei Z G, Lü S H, Hu Z Y, et al. 2005. A primary research on the characteristics of wind, temperature and humidity in the boundary layer over Jinta summer. Plateau Meteorology, 24(6): 846–856. (in Chinese)

    Google Scholar 

  • Wen Y T, Miao Q L, He Q, et al. 2010. Observations on turbulence intensity and turbulent kinetic energy of surface layer in spring and summer in Taklimakan hinterland. Journal of Desert Research, 30(2): 439–444. (in Chinese)

    Google Scholar 

  • Xu X D, Wang Y J, Wei W S, et al. 2014. Summertime precipitation process and atmospheric water cycle over Tarim Basin under the specific large terrain background. Desert and Oasis Meteorology, 8(2): 1–11. (in Chinese)

    Google Scholar 

  • Zhang Q. 2007. Study on depth of atmospheric thermal boundary layer in extreme arid desert regions. Journal of Desert Research, 27(4): 614–620. (in Chinese)

    Google Scholar 

  • Zhang Q, Zhao Y D, Wang S, et al. 2007. A study on atmospheric thermal boundary layer structure in extremely arid desert and gobi region on the clear day in summer. Advances in Earth Science, 22(11): 1150–1159. (in Chinese)

    Google Scholar 

  • Zhang Q, Wang S. 2008. A study on atmospheric boundary layer structure on a clear day in the arid region in northwest China. Acta Meteorologica Sinica, 66(4): 599–608. (in Chinese)

    Google Scholar 

  • Zhang Q, Zhang J, Qiao J, et al. 2011. Relationship of atmospheric boundary layer depth with thermodynamic processes at the land surface in arid regions of China. Science China Earth Sciences, 54(10): 1586–1594.

    Article  Google Scholar 

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Authors and Affiliations

  1. Institute of Desert Meteorology, China Meteorological Administration, Urumqi, 830002, China

    Minzhong Wang, Wenshou Wei, Qing He, Lei Fan & Jiantao Zhang

  2. Taklimakan Desert Atmospheric Environment Observation Experimental Station, Tazhong, 841000, China

    Minzhong Wang, Wenshou Wei, Qing He, Lei Fan & Jiantao Zhang

  3. School of Geographic Science and Tourism, Xinjiang Normal University, Urumqi, 830054, China

    Yuhui Yang

Authors
  1. Minzhong Wang
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  2. Wenshou Wei
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  3. Qing He
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  4. Yuhui Yang
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  5. Lei Fan
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  6. Jiantao Zhang
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Correspondence to Minzhong Wang.

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Wang, M., Wei, W., He, Q. et al. Summer atmospheric boundary layer structure in the hinterland of Taklimakan Desert, China. J. Arid Land 8, 846–860 (2016). https://doi.org/10.1007/s40333-016-0054-3

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  • DOI: https://doi.org/10.1007/s40333-016-0054-3

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