(CCSM4), the IOBM is categorized into three types: the first type can persist until August; the second type transforms from the positive (negative) IOBM into the negative (positive) Indian Ocean Dipole Mode (IODM), accompanied by the El Nio-to-La Nia (La Nia-to-El Nio) transition in ...
However, the NAO-related geopotential height anomalies during the mei-yu onset stage were weak over East Asia and there were distinct differences with the anomalous dipole mode in 2020 over the Atlantic (Fig. 3(a) and Fig. S3(c)). Thus, the impact of the NAO on the mei-yu onset was...
“Once they start attacking that far out,you’re not even really talking about the Somali basin or areas of water that have any connection with Somalia,” said an officer,Roger Middleton.“Once you’re that far out,it’s just the Indian Ocean,and it means you’re looking at trade going...
A universal redux version of my Meteor attempt at Words with Friends (online scrabble). - words-with-strangers-redux/input_words.txt at master · joshwcomeau/words-with-strangers-redux
This manuscript builds on that body of work but is focussed on Southern Ocean algorithms applicable at the basin scale. [5] In this manuscript, our goals are to: [6] 1. Quantify the accuracy of existing satellite chlorophyll algorithms for SeaWiFS (OC4v6), MODIS (OC3M), and GlobColour ...
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Interactions among the Pacific, Atlantic and Indian Oceans through ocean–atmosphere coupling can initiate and/or modulate climate variability. The Pa
Banerjee R, Mukhopadhyay R (1991) Nature and distribution of manganese nodules from three sediment domains of the Central Indian Basin, Indian Ocean. Geo-Mar Lett 11(1):39–43. : 10.1007/BF02431053Banerjee R, Mukhopadhyay, R (1991) Nature and distribution of manganese nodules from three ...
The collision between India and Eurasia mobilizes multiple processes of continental tectonics. However, how deformation develops within the lithosphere across the Tibetan Plateau is still poorly known and a synoptic view is missing. Here, we exploit an e
Indian Ocean (IO) by a dry zone around the eastern IO (EIO), while only the type-I can move out the IO and circulate around the globe. The type-III initiates over the western Pacific (WP) and can circulate the globe. The strong upper-level equatorial westerly wind over the IO-WP,...