Tao L, Cheng S C. 2012. Impact of Indian Ocean basin warming and ENSO on tropical cyclone activities over the western Pacific (in Chinese with English abstract). Chin J Atmos Sci, 36: 1223-1235Tao L, Cheng S C. 2012. Impact of Indian Ocean basin warming and ENSO on tropical cyclone ...
et al. Factors affecting the 2019 Atlantic hurricane season and the role of the Indian Ocean Dipole. Geophys. Res. Lett. 47, e2020GL087781 (2020). Article Google Scholar Zheng, X.-T. et al. Indian Ocean Dipole response to global warming in the CMIP5 multimodel ensemble. J. Clim. ...
Over the past century, the subpolar North Atlantic experienced slight cooling or suppressed warming, relative to the background positive temperature trends, often dubbed the North Atlantic warming hole (NAWH). The causes of the NAWH remain under debate. Here we conduct coupled ocean-atmosphere sim...
Climate Prediction Center’s daily grid precipitation data is used to analyze the spatial–temporal change of extreme precipitation in the Tianshan Mountains from late spring to early summer (May and June), as well as the mechanism of the Indian Ocean Basin Mode (IOBM) on extreme precipitation....
Warming in the TIO has been basin-wide but spatially non-uniform, with the largest increasing trends seen in the central equatorial Indian Ocean and lowest warming trends off the Sumatra and Java coasts. While long-term warming (1900–2015) is maximum over the western Indian Ocean (Roxy et ...
aHomogeneous climate regions in Pakistan 同类的气候地区在巴基斯坦[translate] ai2M xi subcontracted. i2M被转包的XI。[translate] aResponse of the Indian Ocean Basin Mode and Its Capacitor Effect to Global Warming 印度洋盆地方式和它的电容器作用的反应对全球性变暖[translate]...
This study focuses on future change of the Indian Ocean basin-wide (IOBW) and dipole (IOD) modes together with a long-term trend under anthropogenic global warming. That has been investigated using 20 coupled models that participated in Coupled Model Intercomparison Project Phase 5 (CMIP 5) by...
Over the past half a century, both the Indian Ocean (IO) and the North Atlantic Ocean (NA) exhibit strong warming trends like a global mean surface temperature (SST). Here, we show that not only simply as a result of increased greenhouse gases, but the I
Oceanwarminginducesrobustclimaticanomaliesinthe summerIndo-WestPacificregion,prolongingtheElNin˜o’s influenceaftertropicalEastPacificseasurfacetemperature hasreturnedtonormal.InresponsetotheIndianOcean warming,precipitationincreasesovermostofthebasin, forcingaMatsuno-Gillpatternintheuppertroposphere ...
The Indian Ocean Dipole (IOD) is a major climate variability mode that substantially influences weather extremes and climate patterns worldwide. However, the response of IOD variability to anthropogenic global warming remains highly uncertain. The latest