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

is essentially a convectively active envelope that develops over the Indian Ocean and slowly propagates eastward. Because the MJO has such an important influence on the rainfall over the Maritime Continent (e.g., Tian et al. 2006 ; Suzuki 2009 ; Fujita et al. 2011 ; Oh et al. 2012 ; Hagos et al. 2016 ; Sakaeda et al. 2017 ; Kerns and Chen 2018 ), and, more generally, on the weather of the planet (see, among many others, Kiladis and Weickmann 1992 ; Mo 2000 ; Higgins et al. 2000

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

in order to test the study objectives, which are as follows: To assess the dynamic origins of diurnal gravity waves in the MC region and the specific role of orography for these waves. To quantify the nonlinear response to the synchronized diurnal forcing of Borneo and Sumatra. 2. Methodology The regional cloud-permitting numerical model framework of this study is based on that of Wang et al. (2015) , who invoked the Weather Research and Forecasting (WRF) Model, version 3.4.1 ( Skamarock et al

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