Article Contents

EFFECTS OF SEA SURFACE TEMPERATURE AND ITS DIURNAL VARIATION ON DIURNAL VARIATION OF RAINFALL: A PARTITIONING ANALYSIS BASED ON SURFACE RAINFALL BUDGET

Funding:

  • The effects of sea surface temperature (SST) and its diurnal variation on diurnal variation of rainfall are examined in this study by analyzing a series of equilibrium cloud-resolving model experiments which are imposed with zero large-scale vertical velocity. The grid rainfall simulation data are categorized into eight rainfall types based on rainfall processes including water vapor convergence/divergence, local atmospheric drying/moistening, and hydrometeor loss/convergence or gain/divergence. The rainfall contributions of the rainfall types with water vapor convergence are insensitive to the increase in SST from 27℃ to 29℃ during the nighttime, whereas they are decreased during the daytime. The rainfall contributions of the rainfall types with water vapor convergence are decreased as the SST increases from 29℃ to 31℃ but the decreases are larger during the nighttime than during the daytime. The rainfall contributions of the rainfall types with water vapor convergence are decreased by the inclusion of diurnal variation of SST with diurnal difference of 1℃ during the nighttime, but the decreases are significantly slowed down as the diurnal difference of SST increases from 1℃ to 2℃. The rainfall contributions of the rainfall types with water vapor convergence are insensitive to the inclusion of diurnal variation of SST during the daytime.
  • [1] KRAUS E B. The diurnal precipitation changeover the sea [J]. J. Atmos. Sci., 1963, 20(6): 546-551.
    [2] GRAY W M, Jacobson R W. Diurnal variation ofdeep cumulus convection [J]. Mon. Wea. Rev., 1977,105(9): 1171-1188.
    [3] RANDALL D A, Harshvardhan, Dazlich D A. Diurnal variability of the hydrologic cycle in a general circulation model [J]. J. Atmos. Sci., 1991, 48(1):40-62.
    [4] SUI C H, LAU K M. Multiscale phenomena in the tropical atmosphere over the western Pacific [J]. Mon.Wea. Rev., 1992, 120(3): 407-430.
    [5] TAO W K, LANG S, SIMPSON J, et al.Mechanisms of cloud-radiation interaction in thetropics and midlatitudes [J]. J. Atmos. Sci., 1996,53(18): 2624-2651.
    [6] SUI C H, LAU K M, TAKAYABU Y N, et al.Diurnal variations in tropical oceanic cumulusconvection during TOGA COARE [J]. J. Atmos. Sci.,1997, 54(5): 639-655.
    [7] SUI C H, LI X F, LAU K M. Radiative-convective processes in simulated diurnal variations of tropicaloceanic convection [J]. J. Atmos. Sci., 1998, 55(13):2345-2357.
    [8] LIU C, MONCRIEFF M W. A numerical study ofthe diurnal cycle of tropical oceanic convection [J]. J.Atmos. Sci., 1998, 55(13): 2329-2344.
    [9] YANG S, KUO K S, SMITH E A. Persistentnature of secondary diurnal modes of precipitationover oceanic and continental regions [J]. J. Climate,2008, 21(16): 4115-4131.
    [10] CUI X P. A cloud-resolving modeling study ofdiurnal variations of tropical convective andstratiform rainfall [J]. J. Geophys. Res., 2008, 113,D02113, doi: 10.1029/2007JD008990.
    [11] CUI X P, LI X F. Diurnal responses of tropicalconvective and stratiform rainfall to diurnally varyingsea surface temperature [J]. Meteor. Atmos. Phys.,2009, 104(1): 53-61.
    [12] GAO S T, CUI X P, ZHOU Y S et al. Surfacerainfall processes as simulated in a cloud resolvingmodel [J]. J. Geophys. Res., 2005, 110, D10202, doi:10.1029/2004JD005467.
    [13] CUI X P. Quantitative diagnostic analysis ofsurface rainfall processes by surface rainfall equation[J]. Chin. J. Atmos. Sci., 2009, 33(2): 375-387.
    [14] SHEN X, WANG Y, ZHANG N et al. Roles oflarge-scale forcing, thermodynamics, and cloudmicrophysics in tropical precipitation processes [J].Atmos.Res.,2010,doi:10.1016/j.atmosres.2010.04.014.
    [15] SHEN X, WANG Y, ZHANG N et al.Precipitation and cloud statistics in the deep tropical convective regime [J]. J. Geophys. Res., 2010, 115,D24205, doi:10.1029/2010JD014481.
    [16] CUI X P, LI X F. Role of surface evaporation insurface rainfall processes[J]. J. Geophys. Res., 2006,111, D17112, doi:10.1029/2005JD006876.
    [17] GAO S, ZHOU Y, Li X. Effects of diurnalvariations on tropical equilibrium states: Atwo-dimensional cloud-resolving modeling study [J].J. Atmos. Sci., 2007, 64(2): 656-664.
    [18] SUI C H, LAU K M, TAO W K et al. Thetropical water and energy cycles in a cumulusensemble model. Part I: Equilibrium climate [J]. J.Atmos. Sci., 1994, 51(5): 711-728.
    [19] LI X, SUI C H, LAU K M et al. Large-scaleforcing and cloud-radiation interaction in the tropicaldeep convective regime [J]. J. Atmos. Sci., 1999,56(17): 3028-3042.
    [20] SOONG S T, OGURA Y. Response of trade wind cumuli to large-scale processes [J]. J. Atmos. Sci.,1980, 37(9): 2035-2050.
    [21] SOONG S T, TAO W K. Response of deeptropical cumulus clouds to Mesoscale processes [J]. J.Atmos. Sci., 1980, 37(9): 2016-2034.
    [22] TAO W K, SIMPSON J. The Goddard CumulusEnsemble model. Part I: Model description [J]. Terr.Atmos. Oceanic Sci., 1993, 4(1): 35-72.
    [23] CHOU M D, KRATZ D P, RIDGWAY W.Infrared radiation parameterization in numericalclimate models [J]. J. Climate, 1991, 4(4): 424-437.
    [24] CHOU M D, SUAREZ M J, HO C H, et al.Parameterizations for cloud overlapping and shortwave single scattering properties for use ingeneral circulation and cloud ensemble models [J]. J.Climate, 1998, 11(2): 202-214.
    [25] CHOU M D, SUAREZ M J. An efficient thermalinfrared radiation parameterization for use in generalcirculation model [R]. NASA Tech. Memo. 1994,104606, Vol. 3, 85pp. [Available fromNASA/Goddard Space Flight Center, Code 913,Greenbelt, MD 20771.
    [26] LIN Y L, FARLEY R D, ORVILLE H D. Bulkparameterization of the snow field in a cloud model[J]. J. Clim. Appl. Meteor., 1983, 22(6): 1065-1092.
    [27] RUTLEDGE S A, HOBBS P V. The mesoscaleand microscale structure and organization of cloudsand precipitation in midlatitude cyclones. VIII: Amodel for the "seeder-feeder" process in warm-frontal rainbands [J]. J. Atmos. Sci., 1983, 40(5): 1185-1206.
    [28] RUTLEDGE S A, HOBBS P V. The mesoscaleand microscale structure and organization of cloudsand precipitation in midlatitude cyclones. XII: Adisgnostic modeling study of precipitationdevelopment in narrow cold-frontal rainbands [J]. J.Atmos. Sci., 1984, 41(20): 2949-2972.
    [29] TAO W K, SIMPSON J, McCUMBER M. Anice-water saturation adjustment [J]. Mon. Wea. Rev.,1989, 117(1): 231-235.
    [30] KRUEGER S K, FU Q, LIOU K N, et al.Improvement of an ice-phase microphysics parameterization for use in numerical simulations oftropical convection [J]. J. Appl. Meteor., 1995, 34(1):281-287.
    [31] GAO S T, LI X F. Cloud-resolving modeling ofconvective processes [M]. 2008, Dordrecht: Springer,206pp.
    [32] TAO W K, SIMPSON J, SUI C H, et al. Heating,moisture and water budgets of tropical andmidlatitude squall lines: Comparisons and sensitivityto longwave radiation [J]. J. Atmos. Sci., 1993, 50(5):673-690.

Get Citation+

CUI Xiao-peng, Xiaofan LI. EFFECTS OF SEA SURFACE TEMPERATURE AND ITS DIURNAL VARIATION ON DIURNAL VARIATION OF RAINFALL: A PARTITIONING ANALYSIS BASED ON SURFACE RAINFALL BUDGET [J]. Journal of Tropical Meteorology, 2012, 18(1): 89-97.
CUI Xiao-peng, Xiaofan LI. EFFECTS OF SEA SURFACE TEMPERATURE AND ITS DIURNAL VARIATION ON DIURNAL VARIATION OF RAINFALL: A PARTITIONING ANALYSIS BASED ON SURFACE RAINFALL BUDGET [J]. Journal of Tropical Meteorology, 2012, 18(1): 89-97.
Export:  

Share Article

Manuscript History

Manuscript received: 20 December 2010
Manuscript revised: 16 December 2011
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

EFFECTS OF SEA SURFACE TEMPERATURE AND ITS DIURNAL VARIATION ON DIURNAL VARIATION OF RAINFALL: A PARTITIONING ANALYSIS BASED ON SURFACE RAINFALL BUDGET

Abstract: The effects of sea surface temperature (SST) and its diurnal variation on diurnal variation of rainfall are examined in this study by analyzing a series of equilibrium cloud-resolving model experiments which are imposed with zero large-scale vertical velocity. The grid rainfall simulation data are categorized into eight rainfall types based on rainfall processes including water vapor convergence/divergence, local atmospheric drying/moistening, and hydrometeor loss/convergence or gain/divergence. The rainfall contributions of the rainfall types with water vapor convergence are insensitive to the increase in SST from 27℃ to 29℃ during the nighttime, whereas they are decreased during the daytime. The rainfall contributions of the rainfall types with water vapor convergence are decreased as the SST increases from 29℃ to 31℃ but the decreases are larger during the nighttime than during the daytime. The rainfall contributions of the rainfall types with water vapor convergence are decreased by the inclusion of diurnal variation of SST with diurnal difference of 1℃ during the nighttime, but the decreases are significantly slowed down as the diurnal difference of SST increases from 1℃ to 2℃. The rainfall contributions of the rainfall types with water vapor convergence are insensitive to the inclusion of diurnal variation of SST during the daytime.

CUI Xiao-peng, Xiaofan LI. EFFECTS OF SEA SURFACE TEMPERATURE AND ITS DIURNAL VARIATION ON DIURNAL VARIATION OF RAINFALL: A PARTITIONING ANALYSIS BASED ON SURFACE RAINFALL BUDGET [J]. Journal of Tropical Meteorology, 2012, 18(1): 89-97.
Citation: CUI Xiao-peng, Xiaofan LI. EFFECTS OF SEA SURFACE TEMPERATURE AND ITS DIURNAL VARIATION ON DIURNAL VARIATION OF RAINFALL: A PARTITIONING ANALYSIS BASED ON SURFACE RAINFALL BUDGET [J]. Journal of Tropical Meteorology, 2012, 18(1): 89-97.
Reference (32)

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return