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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

typhoons (e.g., Kunze 1985 ; Hormann et al. 2014 ; Baranowski et al. 2014 ). Rather, it is the generation and propagation of near-inertial oscillations driven in response to typhoon forcing that likely most impacts the velocity structure ( Price 1981 ). Such direct velocity measurements of near-inertial motions driven by typhoons are relatively uncommon and are still poorly understood and modeled. The PISTON observations offer a rare glimpse of these features that might help to improve the

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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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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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