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      Relevance of climatological information on spatial and temporal variability of Indian Summer monsoon rainfall (ISMR) in recent El Niño years and its impact on four important kharif crops over India

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      Climate Services
      Elsevier BV

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          A dipole mode in the tropical Indian Ocean.

          For the tropical Pacific and Atlantic oceans, internal modes of variability that lead to climatic oscillations have been recognized, but in the Indian Ocean region a similar ocean-atmosphere interaction causing interannual climate variability has not yet been found. Here we report an analysis of observational data over the past 40 years, showing a dipole mode in the Indian Ocean: a pattern of internal variability with anomalously low sea surface temperatures off Sumatra and high sea surface temperatures in the western Indian Ocean, with accompanying wind and precipitation anomalies. The spatio-temporal links between sea surface temperatures and winds reveal a strong coupling through the precipitation field and ocean dynamics. This air-sea interaction process is unique and inherent in the Indian Ocean, and is shown to be independent of the El Niño/Southern Oscillation. The discovery of this dipole mode that accounts for about 12% of the sea surface temperature variability in the Indian Ocean--and, in its active years, also causes severe rainfall in eastern Africa and droughts in Indonesia--brightens the prospects for a long-term forecast of rainfall anomalies in the affected countries.
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            ENSO control on the south Asian monsoon through the length of the rainy season

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              nasapower: A NASA POWER Global Meteorology, Surface Solar Energy and Climatology Data Client for R

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                Author and article information

                Contributors
                Journal
                Climate Services
                Climate Services
                Elsevier BV
                24058807
                April 2023
                April 2023
                : 30
                : 100370
                Article
                10.1016/j.cliser.2023.100370
                4ada04c2-78a9-474e-9f5c-2f14c2986aa2
                © 2023

                https://www.elsevier.com/tdm/userlicense/1.0/

                http://creativecommons.org/licenses/by-nc-nd/4.0/

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