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On the Relative Role of East and West Pacific Sea Surface Temperature (SST) Gradients in the Prediction Skill of Central Pacific NINO3.4 SST

Autor: S, Lekshmi, Chattopadhyay, Rajib, Pai, D. S., Rajeevan, M., Valsala, Vinu, Hosalikar, K. S., Mohapatra, M.

Dominant modes of SST in the west and east Pacific show strong but regionally different gradients caused by waves, internal dynamics, and anthropogenic warming, which drives air-sea interaction in the Pacific. The study discusses the relative contrib

Externí odkaz: http://arxiv.org/abs/2302.11357

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Large Scale Features of Southwest Monsoon During 2015

Autor: Varikoden, Hamza, Singh, Bhupendra Bahadur, Sooraj, K. P., Joshi, Manish K., Bhaskar, Preethi, Mujumdar, Milind, Rajeevan, M.

Publikováno v: ESSO/IITM/SERP/SR/02(2015)/185, pp 2-13

During 2015, the southwest monsoon (SWM) rainfall over the country remained deficient with seasonal rainfall of about 86% of the long period average (Table 1.1). Last year, the seasonal rainfall deficiency over the country as a whole was 12% (www.imd

Externí odkaz: http://arxiv.org/abs/2012.10385

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A short perspective on the Mascarene High and the abnormal Indian Monsoon during 2015

Autor: Krishnan, R., Singh, Bhupendra, Vellore, R., Mujumdar, M., Swapna, P., Choudhury, Ayantika, Singh, Manmeet, Preethi, B., Rajeevan, M.

Publikováno v: Indian Ocean Bubble (2015), Issue No. 4, pp. 17-19

The initiation of the Indian summer monsoon circulation during late May / early June arises through large-scale land-sea thermal contrast and setting up of negative pressure gradient between the Monsoon Trough over the Indo-Gangetic plains and the Ma

Externí odkaz: http://arxiv.org/abs/2011.11372

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