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  • Air–Sea Interactions from the Diurnal to the Intraseasonal during the PISTON, MISOBOB, and CAMP2Ex Observational Campaigns in the Tropics x
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Adam H. Sobel, Janet Sprintall, Eric D. Maloney, Zane K. Martin, Shuguang Wang, Simon P. de Szoeke, Benjamin C. Trabing, and Steven A. Rutledge

( Fairall et al. 1996 ). Downwelling solar and thermal infrared radiative fluxes were measured by radiometers on the ship. Upwelling radiative fluxes from the surface were modeled using a constant emissivity (0.97) and the Payne (1972) ocean surface albedo parameterization. Precipitation rate is measured with an Optical Scientific, Inc. optical rain gauge. Most meteorological variables were sampled each second, quality controlled, and then averaged to 10-min means. Oceanic temperature and salinity

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Wei-Ting Chen, Chien-Ming Wu, and Hsi-Yen Ma

McFarlane 1995 ; Neale et al. 2008 ), the double-moment microphysics scheme ( Morrison and Gettelman 2008 ; Gettelman et al. 2010 ), the diagnostic cloud fraction (macrophysics) scheme ( Park et al. 2014 ), the shallow convection scheme ( Park and Bretherton 2009 ), the moist turbulence scheme ( Bretherton and Park 2009 ), the Rapid Radiative Transfer Model for GCMs (RRTMG) ( Iacono et al. 2008 ), and the modal aerosol model ( Liu et al. 2012 ). The 3-day-long hindcasts were initialized at 0000 UTC

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