Yanai M, Esbensen S, Chu J H. Determination of average bulk properties of tropical cloud clusters from larger-scale heat and moisture budgets[J]. J Atmos Sci, 1973, 30(4): 611-627. 2.0.CO;2 target="_blank">
Liu C, Ikeda K, Thompson G, et al. High-resolution simulations of wintertime precipitation in the Colorado headwaters region: Sensitivity to physics parameterizations[J]. Mon Wea Rev, 2011, 139: 3533-3553.
Rosen R D, Salstein D A, Peixoto J P. Variability in the annual fields of large-scale atmospheric water vapor transport[J]. Mon Wea Rev, 1979, 107: 26-37. 2.0.CO;2 target="_blank">
[18]
Trenberth K E. Climate diagnostics from global analyses: Conservation of mass in ECMWF analyses[J]. J Climate, 1991, 4: 707-722. 2.0.CO;2 target="_blank">
[19]
Gutowski W J, Chen Y, ？tles Z. Atmospheric water vapor transport in NCEP/NCAR reanalyses: Comparison with river discharge in the central United States[J]. Bull Amer Meteor Soc, 1997, 78: 1957-1969. 2.0.CO;2 target="_blank">
[20]
Roads J, Chen S, Kanamitsu M, et al. Vertical structure of humidity and temperature budget residuals over the Mississippi River basin[J]. J Geophys Res, 1998, 103(D4): 3741-3759.
[21]
Berbery E H, Rasmusson E M. Mississippi moisture budgets on regional scales[J]. Mon Wea Rev, 1999, 127: 2654-2673. 2.0.CO;2 target="_blank">
[22]
Berbery E H, Luo Y, Mitchell K, et al. Eta model-estimated land surface processes and the hydrologic cycle of the Mississippi basin[J]. J Geophys Res, 2003, 108(D22), 8852, doi:10.1029/2002JD003192.
[23]
Becker E J, Berbery E H. Model simulation of the diurnal cycle and moist surges along the Gulf of California during NAME[J]. J Climate, 2008, 28: 771-787.
[24]
Xu J, Zhang B, Wang M, et al. Diurnal variation of summer precipitation over the Tibetan Plateau: A cloud-resolving simulation[J]. Annales Geophysicae, 2012, 30(11): 1575-1586.
[25]
Sato T, Yoshikane T, Satoh M, et al. Resolution dependency of the diurnal cycle of convective clouds over the Tibetan Plateau in a mesoscale model[J]. J Meteor Soc Japan, 2008, 86: 17-31.
[26]
Klemp J B, Skamarock W C, Dudhia J. Conservative split-explicit time integration methods for the compressible nonhydrostatic equations[J]. Mon Wea Rev, 2007, 135: 2897-2913.
[27]
Mlawer E J, Taubman S J, Brown P D, et al. Radiative transfer for inhomogeneous atmosphere: RRTM, a validated correlated-K model for the longwave[J]. J Geophys Res, 1997, 102(D14): 16663-16682.
[28]
Dudhia J. Numerical study of convection observed during the winter monsoon experiment using a mesoscale two-dimensional model[J]. J Atmos Sci, 1989, 46: 3077-3107. 2.0.CO;2 target="_blank">
[29]
Hong S Y, Lim J O J. The WRF Single-Moment 6-Class Microphysics Scheme (WSM6)[J]. J Korean Meteor Soc, 2006, 42: 129-151.
[30]
Chen F, Dudhia J. Coupling an advanced landsurface-hydrology model with the Penn State-NCAR MM5 modeling system. Part I: Model implementation and sensitivity[J]. Mon Wea Rev, 2001, 129: 569-585. 2.0.CO;2 target="_blank">
[31]
Kain J S. The Kain-Fritsch convective parameterization: An update[J]. J Appl Meteor, 2004, 43: 170-181. 2.0.CO;2 target="_blank">
[32]
Huffman G J, Adler R F, Bolvin D, et al. The TRMM multi-satellite precipitation analysis: Quasi-global, multi-year, combined-sensor precipitation estimates at fine scale[J]. J Hydrometeor, 2007, 8(1): 38-55.
[33]
Liu X, Bai A, Liu C. Diurnal variations of summertime precipitation over the Tibetan Plateau in relation to orographically-induced regional circulations[J]. Environ Res Lett, 2009, 4: 045203, doi:10.1088/1748-9326/4/4/045203.
