Rapid 21st Century Warming in the Southern Subtropical Indian Ocean Driven by Altered Inter‐Basin Connections
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2025
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Details
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Journal Title:International Journal of Climatology
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Personal Author:
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NOAA Program & Office:
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Description:The Indian Ocean has been warming rapidly over the last few decades. However, this warming has not been uniform, with the southern subtropical Indian Ocean (STIO, 15°S–35°S) cooling until the late 20th century and then warming abruptly. We show that the Indonesian Throughflow (ITF) into the Indian Ocean exhibits strong decadal variability with a weaker negative trend over the recent decades, and hence cannot explain the continued heat gain by the upper ocean of the STIO at a rate of 0.41 (± 0.02) × 1022 J/decade. An increased ITF during the hiatus in global surface warming initiated the STIO warming, resulting in a weaker Mascarene high and its decoupling from the Southern Ocean atmospheric variability. This enhanced Tasman inflow into the Indian Ocean and weakened Agulhas outflow offsetting the recently weakened ITF, caused a positive feedback that continued to warm the upper ocean of the STIO.
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Source:International Journal of Climatology, 46(1)
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Series:PMEL contribution no. 5587
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DOI:
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ISSN:0899-8418 ; 1097-0088
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Rights Information:Accepted Manuscript
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Compliance:Submitted
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Main Document Checksum:urn:sha-512:2137ada0e52f11310455dcad8ded3a30c67549c639305274fe10df95b5a842b57c32acec80a49a0f29971e0d6b863b7716538aa19e6173dd0ce35f3b27651bae
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