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Satoru Yokoi, Shuichi Mori, Masaki Katsumata, Biao Geng, Kazuaki Yasunaga, Fadli Syamsudin, Nurhayati, and Kunio Yoneyama

convection during nighttime. Warner et al. (2003) and Mapes et al. (2003b) proposed that an ascent motion in the lower troposphere, which was due to gravity waves emanating from the nighttime radiative cooling of the elevated terrain of the Andes, destabilized the offshore atmosphere west of the Pacific coast of Panama and Columbia. Love et al. (2011) and Hassim et al. (2016) suggested the role of gravity waves emanating from convective systems over land. While diabatic heating within convective

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Claire L. Vincent and Todd P. Lane

Continent and scale interaction with the diurnal cycle of precipitation . Quart. J. Roy. Meteor. Soc. , 140 , 814 – 825 , https://doi.org/10.1002/qj.2161 . 10.1002/qj.2161 Rauniyar , S. P. , and K. J. E. Walsh , 2013 : Scale interaction of the diurnal cycle of rainfall over the MC and Australia: Influence of the MJO . J. Climate , 26 , 1304 – 1321 , https://doi.org/10.1175/JCLI-D-12-00124.1 . 10.1175/JCLI-D-12-00124.1 Rotunno , R. , 1983 : On the linear theory of the land and sea breeze

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Satoru Yokoi, Shuichi Mori, Fadli Syamsudin, Urip Haryoko, and Biao Geng

physical processes of the offshore migration and proposed possible mechanisms based on analyses of available observational data such as those from satellites, weather radars, and radiosondes launched from land sites, as well as numerical experiments. Warner et al. (2003) and Mapes et al. (2003b) proposed that gravity waves excited by nighttime radiative cooling of the elevated terrain of the Andes propagated offshore in the lower troposphere and destabilized the offshore atmosphere, contributing to

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