Search Results

You are looking at 1 - 8 of 8 items for :

  • Radiative transfer x
  • Years of the Maritime Continent x
  • All content x
Clear All
Claire L. Vincent and Todd P. Lane

T. Yamada , 1982 : Development of a turbulence closure model for geophysical fluid problems . Rev. Geophys. Space Phys. , 20 , 851 – 875 , https://doi.org/10.1029/RG020i004p00851 . 10.1029/RG020i004p00851 Mlawer , E. J. , S. J. Taubman , P. D. Brown , M. J. Iacono , and S. A. Clough , 1997 : Radiative transfer for inhomogeneous atmospheres: RRTM, a validated correlated-k model for the longwave . J. Geophys. Res. , 102 , 16 663 – 16 682 , https://doi.org/10.1029/97JD

Full access
Giuseppe Torri, David K. Adams, Huiqun Wang, and Zhiming Kuang

significant seasonal shifts in its location ( Wheeler and Kiladis 1999 ). For both simulations, the initial and boundary conditions, as well as SSTs, were provided by ERA-Interim ( Dee et al. 2011 ). Cloud microphysics were parameterized using the WRF Double-Moment (WDM) scheme ( Lim and Hong 2010 ), while radiative transfer was parameterized using the GCM version of the Rapid Radiative Transfer Model (RRTM) longwave radiation scheme ( Iacono et al. 2008 ) and the updated Goddard shortwave scheme ( Chou

Free access
Kevin E. Trenberth and Yongxin Zhang

an El Niño event, and then movement of heat laterally and major adjustments in the vertical distribution of heat and the thermocline during the course of the event as the trade winds relax and the Bjerknes feedback processes kick in. The atmosphere plays a vital role as a bridge among the oceans and to the extratropics through changes in the atmospheric circulation and associated surface fluxes, resulting in a significant diabatic component, as heat is ultimately radiated to space and lost

Open access
James H. Ruppert Jr., Xingchao Chen, and Fuqing Zhang

. J. , J. S. Delamere , E. J. Mlawer , M. W. Shephard , S. A. Clough , and W. D. Collins , 2008 : Radiative forcing by long-lived greenhouse gases: Calculations with the AER radiative transfer models . J. Geophys. Res. , 113 , D13103 , https://doi.org/10.1029/2008JD009944 . 10.1029/2008JD009944 Ichikawa , H. , and T. Yasunari , 2006 : Time–space characteristics of diurnal rainfall over Borneo and surrounding oceans as observed by TRMM-PR . J. Climate , 19 , 1238

Free access
Chu-Chun Chen, Min-Hui Lo, Eun-Soon Im, Jin-Yi Yu, Yu-Chiao Liang, Wei-Ting Chen, Iping Tang, Chia-Wei Lan, Ren-Jie Wu, and Rong-You Chien

4, we use the radiative transfer scheme of the modified NCAR Community Climate Model version 3 (CCM3), the nonlocal planetary boundary layer scheme of Holtslag ( Holtslag et al. 1990 ), the ocean flux scheme of Zeng ( Zeng et al. 1998 ), and the Subgrid Explicit Moisture (SUBEX) scheme for the resolved scale precipitation, which are default schemes of RegCM4 ( Giorgi et al. 2012 ) or applied schemes for RegCM4 simulations of the Southeast Asia domain ( Chung et al. 2018 ). We also performed

Open access
Benjamin A. Toms, Susan C. van den Heever, Emily M. Riley Dellaripa, Stephen M. Saleeby, and Eric D. Maloney

most important for driving the aggregation of water vapor anomalies. Another interesting avenue for future research could be to expand or shift the simulation domain to test whether a similar relationship holds across the rest of the Indo-Pacific region. Additional upscale influences may arise from cloud-radiative feedbacks, since changes in the distribution of cloud have been shown to impact the propagation and intensity of the intraseasonal structure of the MJO ( Flatau et al. 1997 ; Arnold and

Free access
Claire L. Vincent and Todd P. Lane

.1029/RG020i004p00851 . 10.1029/RG020i004p00851 Mitchell , K. , and Coauthors , 2005 : The Community Noah Land-Surface Model (LSM) user’s guide version 2.7.1. NCEP/EMC Tech. Rep., 26 pp. Mlawer , E. J. , S. J. Taubman , P. D. Brown , M. J. Iacono , and S. A. Clough , 1997 : Radiative transfer for inhomogeneous atmospheres: RRTM, a validated correlated-k model for the longwave . J. Geophys. Res. , 102 , 16 663 – 16 682 , doi: 10.1029/97JD00237 . 10.1029/97JD00237 Nakanishi , M

Full access
D. Argüeso, R. Romero, and V. Homar

-only grid cells, only provides first-approach information on the model rainfall realism. Thus, we also examine the precipitation diurnal cycle, which requires the model to better represent local forcing and local circulation in order to capture it. In the MC rainfall has a very distinct diurnal cycle, especially over the islands. Differential solar radiative heating between different surface types causes local pressure gradients that result in land–sea-breeze circulations, which, in combination with

Open access