Abstract
The spatial and temporal global distribution of deep clouds was analyzed using a four-year dataset (2007–10) based on observations from CloudSat and CALIPSO. Results showed that in the Northern Hemisphere, the number of deep cloud systems (DCS) reached a maximum in summer and a minimum in winter. Seasonal variations in the number of DCS varied zonally in the Southern Hemisphere. DCS occurred most frequently over central Africa, the northern parts of South America and Australia, and Tibet. The mean cloud-top height of deep cloud cores (TDCC) decreased toward high latitudes in all seasons. DCS with the highest TDCC and deepest cores occurred over east and south Asian monsoon regions, west-central Africa and northern South America. The width of DCS (WDCS) increased toward high latitudes in all seasons. In general, DCS were more developed in the horizontal than in the vertical direction over high latitudes and vice versa over lower latitudes. Findings from this study show that different mechanisms are behind the development of DCS at different latitudes. Most DCS at low latitudes are deep convective clouds which are highly developed in the vertical direction but cover a relatively small area in the horizontal direction; these DCS have the highest TDCC and smallest WDCS. The DCS at midlatitudes are more likely to be caused by cyclones, so they have less vertical development than DCS at low latitudes. DCS at high latitudes are mainly generated by large frontal systems, so they have the largest WDCS and the smallest TDCC.
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References
Albrecht, B. A., 1989: Aerosols, cloud microphysics, and fractional cloudiness. Science, 245, 1227–1230.
Andreae, M. O., D. Rosenfeld, P. Artaxo, A. A. Costa, G. P. Frank, K. M. Longo, and M. A. F. Silva-Dias, 2004: Smoking rain clouds over the Amazon. Science, 303, 1337–1342.
Freud, E., and D. Rosenfeld, 2012: Linear relation between convective cloud drop number concentration and depth for rain initiation. J. Geophys. Res., 117, D02207, doi:10.1029/2011JD016457.
Futyan, J. M., and A. D. Del Genio, 2007: Deep convective system evolution over Africa and the tropical Atlantic. J. Climate, 20, 5041–5060.
Harrison, E. F., P. Minnis, B. R. Barkstrom, V. Ramanathan, R. D. Cess, and G. G. Gibson., 1990: Seasonal-variation of cloud radiative forcing derived from the Earth Radiation Budget Experiment. J. Geophys. Res., 95(D11), 18 687–18 703.
Hartmann, D. L., M. E. Ockert-Bell, and M. L. Michelsen, 1992: The effect of cloud type on earths’ energy-balance: Global analysis. J. Climate, 5, 1281–1304.
Hartmann, D. L., L. A. Moy, and Q. Fu, 2001: Tropical convection and the energy balance at the top of the atmosphere. J. Climate, 14, 4495–4511.
Huang, J. P., P. Minnis, B. Lin, Y. H. Yi, M. M. Khaiyer, R. F. Arduini, A. Fan, and G. G. Mace, 2005: Advanced retrievals of multilayered cloud properties using multispectral measurements. J. Geophys. Res., 110(D15), D15S18, doi:10.1029/2004JD005101.
Huang, J. P., P. Minnis, B. Lin, Y. H. Yi, T. F. Fan, S. Sun Mack, and J. K. Ayers, 2006: Determination of ice water path in ice-over-water cloud systems using combined MODIS and AMSR-E measurements. Geophys. Res. Lett., 33(21), L21801, doi:10.1029/2006GL027038.
Iwasaki, S., T. Shibata, J. Nakamoto, H. Okamoto, H. Ishimoto, and H. Kubota, 2010: Characteristics of deep convection measured by using the A-train constellation. J. Geophys. Res., 115, D06207, doi:10.1029/2009JD013000.
Khain, A., D. Rosenfeld, and A. Pokrovsky, 2005: Aerosol impact on the dynamics and microphysics of deep convective clouds. Quart. J. Roy. Meteor. Soc., 131, 2639–2663, doi: 10.1256/qj.04.62.
Kiehl, J. T., 1994: On the observed near cancellation between longwave and shortwave cloud forcing in tropical regions. J. Climate, 7, 559–565.
Koren, I., Y. J. Kaufman, D. Rosenfeld, L. A. Remer, and Y. Rudich, 2005: Aerosol invigoration and restructuring of Atlantic convective clouds. J. Geophys. Res., 32, L14828, doi:10.1029/2005GL023187.
Lee, S. S., L. Donner, and J. E. Penner, 2010: Thunderstorm and stratocumulus: How does their contrasting morphology affect their interactions with aerosols? Atmos. Chem. Phys., 10, 6819–6837, doi: 10.5194/acp-10-6819-2010.
Luo, Y. L., R. H. Zhang, W. M. Qian, Z. Z. Luo, and H. Xin, 2010: Intercomparison of deep convection over the Tibetan Plateau-Asian monsoon region and subtropical North America in boreal summer using CloudSat/CALIPSO data. J. Climate, 24, 2164–2177, doi:10.1175/2009JCLI4032.1.
Niu, F., and Z. Q. Li, 2012: Systematic variations of cloud top temperature and precipitation rate with aerosols over the global tropics. Atmos. Chem. Phys., 12, 8491–8498, doi:10.5194/acp-12-84910-2012.
Li, Z. Q., F. Niu, J. W. Fan, Y. G. Liu, D. Rosenfeld, and Y. N. Ding, 2011: Long-term impacts of aerosols on the vertical development of clouds and precipitation. Nat. Geosci., 4, 888–894, doi: 10.1038/ngeo1313.
Peng, J., H. Zhang, and X. Y. Shen, 2013: Analysis of vertical structure of clouds in East Asia with CloudSat data. Chinese J. Atmos. Sci., 37(1), 91–100, doi: 10.3878/j.issn.1006-9895.2012.11188. (in Chinese)
Radke, L. F., J. A. Coakley Jr., and M. D. King, 1989: Direct and remote sensing observations of the effects of ships on clouds. Science, 246, 1146–1149.
Ramanathan, V., R. D. Cess, E. F. Harrison, P. Minnis, B. R. Barkstrom, E. Ahmad, and D. Hartmann, 1989: Cloud-radiative forcing and climate: Results from the Earth Radiation Budget Experiment. Science, 243, 57–63.
Ramanathan, V., P. J. Crutzen, J. T. Kiehl, and D. Rosenfeld, 2001: Aerosols, climate, and the hydrological cycle. Science, 294, 2119–2124.
Rosenfeld, D., 2000: Suppression of rain and snow by urban and industrial air pollution. Science, 287, 1793–1796.
Rosenfeld, D., U. Lohmann, G. B. Rage, C. D. O’Dowd, M. Kulmala, S. Fuzzi, A. Reissell, and M. O. Andreae, 2008: Flood or drought: How do aerosols affect precipitation?. Science, 321, 1309–1313.
Sassen, K., Z. E. Wang, and D. Liu, 2009: Cirrus clouds and deep convection in the tropics: Insights from CALIPSO and CloudSat. J. Geophys. Res., 114, D00H06, doi:10.1029/2009JD011916.
Savtchenko, A., 2009: Deep convection and upper-tropospheric humidity: A look from the A-Train. Geophys. Res. Lett., 36, L06814, doi:10.1029/2009GL037508.
Takahashi, H., and Z. J. Luo, 2012: Where is the level of neutral buoyancy for deepconvection? Geophys. Res. Lett., 39, L15809, doi:10.1029/2012GL052638.
Tao, W. K., X. W. Li, A. Khain, T. Matsui, S. Lang, and J. Simpson, 2007: Role of atmospheric aerosol concentration on deep convective precipitation: Cloud-resolving model simulations. J. Geophys. Res., 112, D24S18, doi:10.1029/2007JD008728.
Yuan, J., and R. A. Houze Jr., 2010: Global variability of mesoscale convective system anvil structure from A-Train satellite data. J. Climate, 23, 5864–5888, doi: 10.1175/2010JCLI3671.1.
Yuan, J., R. A. Houze Jr., and A. J. Heymsfield, 2011: Vertical structures of anvil clouds of tropical mesoscale convective systems observed by CloudSat. J. Atmos. Sci., 68, 1653–1674, doi:10.1175/2011JAS3687.1.
Yuan, T. L., and Z. Q. Li, 2010: General macro- and microphysical properties of deep convective clouds as observed by MODIS. J. Climate, 23, 3457–3473, doi:10.1175/2009JCLI3136.1.
Yuan, T. L., J. V. Martins, Z. Q. Li, and L. A. Remer, 2010: Estimating glaciation temperature of deep convective clouds with remote sensing data. Geophys. Res. Lett., 37, L08808, doi:10.1029/2010GL042753.
Zhang, H., J. Peng, X. W. Jing, and J. N. Li, 2013: The features of cloud overlapping in Eastern Asia and their effect on cloud radiative forcing. Sci. China (Earth), 56, 737–747, doi: 10.1007/s11430-012-4489-x.
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Peng, J., Zhang, H. & Li, Z. Temporal and spatial variations of global deep cloud systems based on CloudSat and CALIPSO satellite observations. Adv. Atmos. Sci. 31, 593–603 (2014). https://doi.org/10.1007/s00376-013-3055-6
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DOI: https://doi.org/10.1007/s00376-013-3055-6