Hong S Y,Noh Y,Dudhia J. A new vertical diffusion package with an explicit treatment of entrainment processes[J]. Mon Wea Rev,2006,134(9):2318-2341.
[2]
Li Tao,Zheng Xiaogu,Dai Yongjiu,et al. Mapping near-surface air temperature,pressure,relative humidity and wind speed over mainland chinawith high spatiotemporal resolution[J].Adv Atmos Sci,2014,31(5):1127-1135.
[3]
Ngo-Duc T,Polcher J,Laval K. A 53-year forcing data set for land surface models[J]. J Geophys Res:Atmos(1984-2012),2005,110(D6),doi:10.1029/2004JD005434.
[4]
Shepard D. A two-dimensional interpolation function for irregularly-spaced data[C]. Proceedings of the 23rd National Conference ACM,New York,ACM Press,1968:517-524.
[5]
Marshall J S, Palmer W M K. The distribution of raindrops with size[J]. J Meteor, 1948, 5(4):165-166. 2.0.CO;2 target="_blank">
[6]
Mlawer E J,Taubman S J,Brown P D,et al. Radiative transfer for inhomogeneous atmosphere:RRTM,a validated correlated-k model for the long-wave[J]. J Geophys Res,1997,102(D14):16663-16682.
[7]
Chou M D,Suarez M J. An efficient thermal infrared radiation parameterization for use in general circulation models[J]. Laboratory for Atmospheres,NASA Tech Memo,1994,85.
[8]
Zhang Huqiang,Bernard Pak,Wang Yingping,et al. Evaluating Surface Water Cycle Simulated by the Australian Community Land Surface Model(CABLE)across Different Spatial and Temporal Domains[J]. Journal of Hydrometeorology,2013,14(4):1119-1138.
[9]
Tokay A, Short D A. Evidence from tropical raindrop spectra of the origin of rain from stratiform versus convective clouds[J]. J Appl Meteor, 1996, 35(3):355-371. 2.0.CO;2 target="_blank">
[10]
Noh Yign,Woo Geun Cheon,Song-You Hon,et al. Improvement of the K-profile model for the planetary boundary layer based on large eddy simulation data[J]. Bound-Layer Meteor,2003,107(2):401-427.
[11]
Uijlenhoet R, Steiner M, Smith J A. Variability of raindrop size distributions in a squall line and implications for radar rainfall estimation[J]. J Hydrometeor, 2003, 4(1):43-61. 2.0.CO;2 target="_blank">
[12]
Schlosser C A,Gao X. Assessing evapotranspiration estimates from the Second Global Soil Wetness Project(GSWP-2) simulations[J]. Journal of Hydrometeorology,2010,11(4):880-897.
Kowalczyk E,Wang Y P,Law R M,et al. CSIRO Atmosphere Biosphere Land Exchange model for use in climate models and as an offline model[R]. CSIRO Marine and Atmospheric Technical report,2007:1-37.
[15]
Chen F,Dudhia J. Coupling an advanced land-surface/hydrology model with the Penn State/NCAR MM5 modeling system. Part I:Model description and implementation[J]. Mon Wea Rev,2001,129(4):569-585. 2.0.CO;2 target="_blank">
[16]
Brawn D, Upton G. Estimation of an atmospheric Gamma drop size distribution using disdrometer data[J]. Atmospheric Research, 2008, 87(1):66-79.
[17]
Zhang Huqiang,Zhang Liang,Pak B. Comparing surface energy,water and carbon cycle in dry and wet regions simulated by a land-surface model[J]. Theor Appl Climatol,2011,104(3-4):511-527.
[18]
Grell G A,Devenyi D. A generalized approach to parameterizing convection combining ensemble and data assimilation techniques[J]. Geophys Res Lett,2002,29(14):381-384.
Zhang Liang,Zhang Huqiang,Li Yaohui. Surface energy,water and carbon cycle in China simulated by the Australian community land surface model(CABLE)[J]. Theor Appl Climatol,2011,96(3-4):375-394.
Wang Y P,R Leuning. A two-leaf model for canopy conductance,photosynthesis and partitioning of available energy I:Model description and comparison with a multi-layered model[J]. Agric For Meteorol,1998,91(2):89-111.
[28]
Ulbrich C W. Natural variations in the analytical form of the raindrop size distribution[J]. J Climate Appl Meteor, 1983, 22(10):1764-1775. 2.0.CO;2 target="_blank">
Raupach M R. A practical Lagrangian method for relating scalar concentrations to source distributions in vegetation canopies[J]. Quart J Roy Meteorol Soc,1989,115(487):609-632.
[32]
Wakasugi K, Mizutani A, Matsuo M, et al. A direct method for deriving drop-size distribution and vertical air velocities from VHF Doppler radar spectra[J]. Journal of Atmospheric and Oceanic Technology, 1986, 3(4):623-629. 2.0.CO;2 target="_blank">
[33]
Raupach M R. Applying Lagrangian fluid mechanics to infer scalar source distributions from concentration profiles in plant canopies[J]. Agric For Meteorol,1989,47(2):85-108.
Ohno Y, Williams C R, Gage K S. Simplified method for rain rate and Z-R relation estimation using UHF wind profiler[C]. 29th International Conference on Radar Meteorology, Montreal, Canada, 1999:4-17.
Keyantash J,Dracup J A. The quantification of drought:An evaluation of drought indices[J]. Bull Amer Meteor Soc,2002,83(8):1167-1180. 2.3.CO;2 target="_blank">
Willis P T. Functional fits to some observed drop size distributions and parameterization of rain[J]. J Atmos Sci, 1984, 41(9):1648-1661. 2.0.CO;2 target="_blank">
[46]
Caracciolo C, Prodi F, Battaglia A, et al. Analysis of the moments and parameters of a Gamma DSD to infer precipitation properties:A convective stratiform discrimination algorithm[J]. Atmos Res, 2006, 80(2):165-186.
[47]
Nzeukou A, Sauvageot H, Ochou A D, et al. Raindrop size distribution and radar parameters at Cape Verde[J]. J Appl Meteor, 2004, 43(1):90-105. 2.0.CO;2 target="_blank">
[48]
Gunn R, Kinzer G D. The terminal velocity of fall for water droplets in stagnant air[J]. Meteor, 1949, 6:243-248. 2.0.CO;2 target="_blank">
[49]
Foote G B, Du Toit P S. Terminal velocity of raindrops aloft[J]. J Appl Meteor, 1969, 8(2):249-253. 2.0.CO;2 target="_blank">
Ulbrich C W, Chilson P B. Effects of variations in precipitation size distribution and fallspeed law parameters on relations between mean Doppler fallspeed and reflectivity factor[J]. Journal of Atmospheric and Oceanic Technology, 1994, 11(6):1656-1663. 2.0.CO;2 target="_blank">
