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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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Corinne B. Trott, Bulusu Subrahmanyam, Heather L. Roman-Stork, V. S. N. Murty, and C. Gnanaseelan

-scale movement of strong cloud convection and precipitation, which directly alters the surface circulation of the BoB, as studied by Grunseich et al. (2011) using altimeter observations. MJOs force equatorial Kelvin waves that propagate northward along the eastern coastline ( Cheng et al. 2013 ). These Kelvin waves can alter the mixed layer variability and directly change the rate of air–sea heat flux in the BoB ( Oliver and Thompson 2010 ). The relationships between the MJO and surface fluxes over the BoB

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Michael B. Natoli and Eric D. Maloney

greater contrast between land and sea due to a difference in thermal inertia, resulting in a strong sea-breeze circulation and more vigorous convection. Surface insolation is strongly reduced by phase 6, providing less forcing for a strong diurnal cycle. Fig . 11. ERA5 (a) daily mean surface downwelling shortwave radiation anomalies by BSISO phase relative to the May–October mean and (b) BSISO anomalies of the diurnal amplitude of surface zonal wind relative to May–October composite diurnal cycle of

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

://doi.org/10.1175/2007JCLI1457.1 . 10.1175/2007JCLI1457.1 Iacono , M. 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 Jakob , C. , and A. P. Siebesma , 2003 : A new subcloud model for mass-flux convection schemes: Influence on triggering

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