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Features of clouds and convection during the pre- and post-onset periods of the Asian summer monsoon

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Abstract

The statistical characteristics of the vertical structure of clouds in the Asian summer monsoon region are investigated using two CloudSat standard products (Geometrical Profiling Product (GEOPROF) and GEOPROF-lidar) during the pre- and post-onset periods of the Asian summer monsoon, from April to August in 2007–2010. The characteristics of the vertical structure of clouds are analyzed and compared for different underlying surfaces in four subregions during this period. Also analyzed are the evolution of precipitation and hydrometeors with the northward advance of the Asian summer monsoon, and different hydrometeor characteristics attributed to the underlying surface features. The results indicate that the vertical cloud amounts increase significantly after the summer monsoon onset; this increase occurs first in the upper troposphere and then at lower altitudes over tropical regions (South Asian and tropical Northwest Pacific regions). The heights of the cloud top ascend, and the vertical height between the top and the base of the whole cloud increases. Single-layer (SL) and double-layer (DL) hydrometeors contribute over half and one third of the cloudiness in these 5 months (April to August), respectively. The multilayer frequencies increase in four different regions, and cloud layer depths (CLD) increase after the summer monsoon onset. These changes are stronger in tropical regions than in subtropical regions, while the vertical distance between cloud layers (VDCL) deceases in tropical regions and increases in subtropical regions.

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References

  • Andermann C, Bonnet S, Gloaguen R (2011) Evaluation of precipitation data sets along the Himalayan front. Geochem Geophys Geosyst 12(7), Q07023

    Article  Google Scholar 

  • Boos WR, Kuang ZM (2010) Dominant control of the South Asian monsoon by orographic insulation versus plateau heating. Nature 463:218–223

    Article  Google Scholar 

  • Chang CP (2004) East Asian Monsoon (Vol. 2). World Scientific, Singapore

    Book  Google Scholar 

  • Cui Y, Wang CH (2009) Comparison of sensible and latent heat fluxes during the transition season over the western Tibetan Plateau from reanalysis datasets. Prog Nat Sci 19(6):719–726

    Article  Google Scholar 

  • Devasthale A, Fueglistaler S (2010) A climatological perspective of deep convection penetrating the TTL during the Indian summer monsoon from the AVHRR and MODIS instruments. Atmos Chem Phys 10:4573–4582

    Article  Google Scholar 

  • Ding Y (2007) The variability of the Asian summer monsoon. J Meteorol Soc Jpn Ser II 85:21–54

    Article  Google Scholar 

  • Ding Y, Chan JC (2005) The East Asian summer monsoon: an overview. Meteorog Atmos Phys 89:117–142

    Article  Google Scholar 

  • Flohn H (1957) Large-scale aspects of the “summer monsoon” in South and East Asia. J Meteorol Soc Jpn 75:180–186

    Google Scholar 

  • Gray WM, Jacobson RW Jr (1977) Diurnal variation of deep cumulus convection. Mon Weather Rev 105:1171–1188

    Article  Google Scholar 

  • Haladay T, Stephens G (2009) Characteristics of tropical thin cirrus clouds deduced from joint CloudSat and CALIPSO observations. J Geophys Res 114:D00A25. doi:10.1029/2008JD010675

    Google Scholar 

  • Haynes JM, Stephens GL (2007) Tropical oceanic cloudiness and the incidence of precipitation: early results from CloudSat. Geophys Res Lett 34, L09811. doi:10.1029/2007GL029335

    Article  Google Scholar 

  • Hendon H, Woodberry K (1993) The diurnal cycle of tropical convection. J Geophys Res 98:16623–16637. doi:10.1029/93JD00525

    Article  Google Scholar 

  • Houze RA, Wilton DC, Smull BF (2007) Monsoon convection in the Himalayan region as seen by the TRMM Precipitation Radar. Q J R Meteorol Soc 133:1389–1411

    Google Scholar 

  • Huffman GJ, Bolvin DT, Nelkin EJ, Wolff DB, Adler RF, Gu G, Hong Y, Bowman KP, Stocker EF (2007) The TRMM Multisatellite Precipitation Analysis (TMPA): quasi-global, multiyear, combined-sensor precipitation estimates at fine scales. J Hydrometeorol 8:38–55

    Article  Google Scholar 

  • Im E, Wu C, Durden SL (2005) Cloud profiling radar for the CloudSat mission. IEEE Trans Aerosp Electon Syst 20:483–486

    Google Scholar 

  • Johnson RH, Ciesielski PE (2002) Characteristics of the 1998 summer monsoon onset over the northern South China Sea. J Meteorol Soc Jpn 80(4):561–578

    Article  Google Scholar 

  • Kuhn WR (1978) The effects of cloud height, thickness, and overlap on tropospheric terrestrial radiation. J Geophys Res 83:1337–1346

    Article  Google Scholar 

  • Lau K, Yang S (1997) Climatology and interannual variability of the Southeast Asian summer monsoon. Adv Atmos Sci 14:141–162

    Article  Google Scholar 

  • Li CF, Yanai M (1996) The onset and interannual variability of the Asian summer monsoon in relation to land–sea thermal contrast. J Clim 9:358–375

    Article  Google Scholar 

  • Liang XZ, Wang WC (1997) Cloud overlap effects on general simulations circulation model climate. J Geophys Res 102:11039–11047

    Article  Google Scholar 

  • Luo Y, Zhang R, Wang H (2009) Comparing occurrences and vertical structures of hydrometeors between eastern China and the Indian monsoon region using CloudSat/CALIPSO data. J Clim 22:1052–1064

    Article  Google Scholar 

  • Luo Y, Zhang R, Qian W, Luo Z, Hu X (2011) Intercomparison of deep convection over the Tibetan Plateau-Asian monsoon region and subtropical North America in boreal summer using CloudSat/CALIPSO data. J Clim 24:2164–2177

    Article  Google Scholar 

  • Mace GG, Marchand R, Zhang Q, Stephens G (2007) Global hydrometeor occurrence as observed by CloudSat: initial observations from summer 2006. Geophys Res Lett 34, L09808. doi:10.1029/2006GL029017

    Article  Google Scholar 

  • Mace GG, Zhang Q, Vaughan M, Marchand R, Stephens G, Trepte C, Winker D (2009) A description of hydrometeor layer occurrence statistics derived from the first year of merged Cloudsat and CALIPSO data. J Geophys Res 114:D00A26. doi:10.1029/2007JD009755

    Google Scholar 

  • Matsumoto J (1997) Seasonal transition of summer rainy season over Indochina and adjacent monsoon region. Adv Atmos Sci 14:231–245

    Article  Google Scholar 

  • Medina S, Houze RA, Kumar A, Niyogi D (2010) Summer monsoon convection in the Himalayan region: terrain and land cover effects. Q J R Meteorol Soc 136:593–616. doi:10.1002/qj.601

    Google Scholar 

  • Meehl GA (1994) Influence of the land surface in the Asian summer monsoon: external conditions versus internal feedbacks. J Clim 7:1033–1049

    Article  Google Scholar 

  • Nesbitt SW, Zipser EJ (2003) The diurnal cycle of rainfall and convective intensity according to three years of TRMM measurements. J Clim 16:1456–1475

    Article  Google Scholar 

  • Nitta T (1983) Observational study of heat sources over the eastern Tibetan Plateau during the summer monsoon. J Meteorol Soc Jpn 61(4):590–605

    Google Scholar 

  • Romatschke U, Houze RA Jr (2011) Characteristics of precipitating convective systems in the South Asian monsoon. J Hydrometeorol 12(1):3–26

    Article  Google Scholar 

  • Romatschke U, Medina S, Houze RA Jr (2010) Regional, seasonal, and diurnal variations of extreme convection in the South Asian region. J Clim 23:419–439

    Article  Google Scholar 

  • Sassen K, Wang Z, Liu D (2009) Cirrus clouds and deep convection in the tropics: insights from CALIPSO and CloudSat. J Geophys Res 114:D00H06. doi:10.1029/2009JD011916

    Google Scholar 

  • Soman MK, Krishna Kumar K (1993) Space-time evolution of meteorological features associated with the onset of Indian summer monsoon. Mon Weather Rev 121(4):1177–1194

    Article  Google Scholar 

  • Stephens GL (2005) Cloud feedbacks in the climate system: a critical review. J Clim 18(2):237–273

    Article  Google Scholar 

  • Stephens GL, Vane DG, Boain RJ, Mace GG, Sassen K, Wang Z, Illingworth AJ, O’Connor EJ, Rossow WB, Durden SL (2002) The CloudSat mission and the A-Train: a new dimension of space-based observations of clouds and precipitation. Bull Am Meteorol Soc 83:1771–1790

    Article  Google Scholar 

  • Tian B, Soden BJ, Wu X (2004) Diurnal cycle of convection, clouds, and water vapor in the tropical upper troposphere: satellites versus a general circulation model. J Geophys Res 109, D10101. doi:10.1029/ 2003JD004117

    Article  Google Scholar 

  • Wang B, Lin H (2002) Rainy season of the Asian-Pacific summer monsoon. J Clim 15:386–398. doi:10.1175/1520-0442(2002)015<0386:RSOTAP>2.0.CO;2

    Article  Google Scholar 

  • Wang B, Zhang Y, Lu M (2004) Definition of South China Sea monsoon onset and commencement of the East Asia summer monsoon. J Clim 17:699–710

    Article  Google Scholar 

  • Wang CH, Shi R, Cui Y, Zuo HC (2009) Simulation analysis on characteristics of land surface over western Qinghai-Xizang Plateau during freezing–thawing period. Sci Cold Arid Reg 1(4):0329–0340

    Google Scholar 

  • Wang CH, Cui Y, Jin SL (2011) Oscillation propagation features of the atmosphere around the Qinghai-Xizang Plateau during the spring season of typical strong and weak monsoon years. Sci China Earth Sci 54:305–314. doi:10.1007/s11430-010-4113-x

    Article  Google Scholar 

  • Wang C, Yu L, Huang B (2012) The impact of warm pool SST and general circulation on increased temperature over the Tibetan Plateau. Adv Atmos Sci 29:274–284

    Article  Google Scholar 

  • Winker DM, Pelon J, McCormick MP (2003) The CALIPSO mission: spaceborne lidar for observation of aerosols and clouds. Proc SPIE Int Soc Opt Eng 4893:1–11

    Google Scholar 

  • Winker DM, Hunt WH, McGill MJ (2007) Initial performance assessment of CALIOP. Geophys Res Lett 34, L19803. doi:10.1029/2007GL030135

    Article  Google Scholar 

  • Wu GX, Liu Y, Zhang Q et al (2007) The influence of the mechanical and thermal forcing of the Tibetan Plateau on the Asian climate. J Hydrometeorol 8:770–789

    Article  Google Scholar 

  • Wu GX, Liu YM, He B, Bao Q, Duan AM, Jin FF (2012) Thermal controls on the Asian summer monsoon. Sci Rep 2:404. doi:10.1038/srep00404

    Google Scholar 

  • 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 Meteorol Soc Jpn 70(1B):319–351

    Google Scholar 

  • Yeh TC, Gao YX (1979) The meteorology of the qinghai-xizang (Tibet) plateau. Science Press, Beijing (in Chinese)

  • Yuter S, Houze RA Jr (1995) Three-dimensional kinematic and microphysical evolution of Florida cumulonimbus. Part II: frequency distributions of vertical velocity, reflectivity, and differential reflectivity. Mon Weather Rev 123:1941–1963

    Article  Google Scholar 

  • Zipser EJ, Cecil DJ, Liu C, Nesbitt SW, Yorty DP (2006) Where are the most intense thunderstorms on earth? Bull Am Meteorol Soc 87:1057–1071

    Article  Google Scholar 

Download references

Acknowledgments

We would like to acknowledge the CloudSat and CALIPSO science teams and engineers, whose efforts and dedication made this study possible. This work was supported by the NSFC (Nos 91337215, 91437217, 41275061, 41471034), China National Basic Research Programme (2013CBA01808). We thank the Meteorology Information Center of the Chinese Meteorology Administration (CMA) for providing observation data, and Gansu Province Super-Computer Center for providing our work environment. We are grateful to Dr. Gerd Bürger for helping to improve the English in the manuscript. We also thank the anonymous reviewer whose suggestions contributed to considerable improvements of the paper.

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Correspondence to Chenghai Wang.

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Wang, Y., Wang, C. Features of clouds and convection during the pre- and post-onset periods of the Asian summer monsoon. Theor Appl Climatol 123, 551–564 (2016). https://doi.org/10.1007/s00704-015-1372-7

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  • DOI: https://doi.org/10.1007/s00704-015-1372-7

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