Results 231 to 240 of about 16,366 (265)

North Indian Ocean tropical cyclone activities influenced by the Indian Ocean Dipole mode

Science China Earth Sciences, 2012
Using Joint Typhoon Warning Center tropical cyclone (TC) track data over the North Indian Ocean (NIO), National Centers for Environmental Prediction monthly reanalysis wind and outgoing long-wave radiation data, and National Oceanic and Atmospheric Administration sea surface temperature data from 1981 to 2010, spatiotemporal distributions of NIO TC ...
JunPeng Yuan, Jie Cao
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Predictability of Indian Ocean Dipole (IOD)

2016
This is an advance summary of a forthcoming article in the Oxford Research Encyclopedia of Climate Science. Please check back later for the full article. The tropical Indian Ocean is unique in several aspects.
openaire   +1 more source

Influence of the Indian Ocean Dipole on the Indian Ocean Meridional Heat Transport

Journal of Marine Systems, 2014
Abstract Influence of the Indian Ocean Dipole (IOD) on the Indian Ocean Meridional Heat Transport (MHT) is studied using 60-yr SODA data. Results show that there is anomalous heat transport from the equatorial region to higher latitudes in both hemispheres during IOD events, and the anomalous poleward MHT occurs mainly in the western Indian Ocean ...
Shuangwen Sun, Yue Fang, Lin Feng, null Tana   +3 more
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Impact of Indian Ocean Dipole on high-frequency atmospheric variability over the Indian Ocean

Atmospheric Research, 2009
A strong relationship between Indian Ocean Dipole (IOD) and high-frequency (HF) atmospheric variability in the low-level zonal wind is reported in the present study. We found that the HF atmospheric variability over the Indian Ocean (IO) is strongly modulated by IOD events, that is, HF atmospheric variability becoming significantly energetic during ...
Jong-Seong Kug, K.P. Sooraj, Fei-Fei Jin, Jing-Jia Luo, Minho Kwon   +4 more
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The Indian Ocean Dipole: A Monopole in SST

Journal of Climate, 2014
Abstract The claim for a zonal-dipole structure in interannual variations of the tropical Indian Ocean (IO) SSTs—the Indian Ocean dipole (IOD)—is reexamined after accounting for El Niño–Southern Oscillation’s (ENSO) influence. The authors seek an a priori accounting of ENSO’s seasonally stratified influence on IO SSTs and evaluate the ...
Sumant Nigam, Yongjing Zhao
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How is the Indian Ocean Subtropical Dipole excited?

Climate Dynamics, 2012
Based on experiments using a coupled general circulation model which resolves tropical ocean–atmosphere coupled phenomena such as El Nino/Southern Oscillation (ENSO) and the Indian Ocean Dipole, forcing mechanisms of the Indian Ocean subtropical dipole (IOSD) are investigated.
Yushi Morioka, Tomoki Tozuka, Toshio Yamagata   +2 more
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INTERANNUAL OSCILLATORY MODES IN THE INDIAN OCEAN AND PREDICTABILITY OF THE INDIAN OCEAN DIPOLE

2011
This study further investigates the 18-month and 3-year variability modes in the Indian Ocean and their possible use for the prediction of the Indian Ocean dipole (IOD). We argue that the IOD is not an isolated event triggered by a particular ocean–atmosphere state but a continuous oscillatory process, so that the extremely shallow thermocline in ...
IRINA V. SAKOVA, RICHARD COLEMAN
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Response of the Indian Ocean Meridional Overturning Circulation to the Subtropical Indian Ocean Dipole

Journal of Climate
Abstract Using the German contribution to Estimating the Circulation and Climate of the Ocean, version 3 (GECCO3), reanalysis data, this work explores the Indian Ocean meridional overturning circulation (IMOC) variability and mechanism during the mature phase of the subtropical Indian Ocean dipole (SIOD). The IMOC is decomposed into the Ekman component,
Linfang Zhang, Marco Yu-Ting Leung, Fengchao Yao, Guangli Zhang, Dongxiao Wang   +4 more
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Air–sea interactions in tropical Indian Ocean: The Indian Ocean Dipole

2021
Swadhin Kumar Behera, Takeshi Doi, J. Venkata Ratnam   +2 more
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Tara Oceans: towards global ocean ecosystems biology

Nature Reviews Microbiology, 2020
Shinichi Sunagawa, Silvia G Acinas, Peer Bork   +2 more
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