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Modelhttps://test-journals.ametsoc.org/view/journals/clim/34/14/JCLI-D-20-0648.1.xmlThe Importance of Central Pacific Meridional Heat Advection to the Development of ENSO2022-01-31https://test-journals.ametsoc.org/view/journals/clim/34/14/JCLI-D-20-0648.1.pdf2022-01-31The Importance of Central Pacific Meridional Heat Advection to the Development of ENSOhttps://test-journals.ametsoc.org/view/journals/clim/34/14/JCLI-D-20-0656.1.xmlFuture Changes in the Frequency of Extreme Droughts over China Based on Two Large Ensemble Simulations2022-01-31https://test-journals.ametsoc.org/view/journals/clim/34/14/JCLI-D-20-0656.1.pdf2022-01-31Future Changes in the Frequency of Extreme Droughts over China Based on Two Large Ensemble Simulationshttps://test-journals.ametsoc.org/view/journals/clim/34/14/JCLI-D-20-0668.1.xmlHeavier Inner-Core Rainfall of Major Hurricanes in the North Atlantic Basin Than in Other Global Basins2022-01-31https://test-journals.ametsoc.org/view/journals/clim/34/14/JCLI-D-20-0668.1.pdf2022-01-31Heavier Inner-Core Rainfall of Major Hurricanes in the North Atlantic Basin Than in Other Global Basinshttps://test-journals.ametsoc.org/view/journals/clim/34/14/JCLI-D-20-0739.1.xmlThe Effect of an Equatorial Continent on the Tropical Rain Belt. 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