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首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >Tropical Indo-Pacific hydroclimate response to North Atlantic forcing during the last deglaciation as recorded by a speleothem from Sumatra, Indonesia
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Tropical Indo-Pacific hydroclimate response to North Atlantic forcing during the last deglaciation as recorded by a speleothem from Sumatra, Indonesia

机译：苏门答腊州苏马特拉的斯派内测量期间对北大西洋迫使北大西洋强迫的热带印度迫使

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摘要

Abrupt changes in Atlantic Meridional Overturning Circulation are known to have affected the strength of the Indian and Asian Monsoons during glacial and deglacial climate states. However, there is still much uncertainty around the hydroclimate response of the Indo-Pacific Warm Pool (IPWP) region to abrupt climate changes in the North Atlantic. Many studies suggest a mean southward shift in the intertropical convergence zone (ITCZ) in the IPWP region during phases of reduced Atlantic meridional overturning, however, existing proxies have seasonal biases and conflicting responses, making it difficult to determine the true extent of North Atlantic forcing in this climatically important region.
机译：众所周知，大西洋经营过度循环的突然变化受到冰川和嗜血气候国家期间印度和亚洲季风的力量。 然而，围绕北方大西洋的气候变化突然存在越来越多的不确定性。 许多研究表明，在大西洋增长的阶段，IPWP地区的闭管会收敛区（ITCZ）中的平均南方转移，然而，现有代理具有季节性偏见和冲突的反应，使得难以确定北大西洋强迫的真实程度 在这个重要的重要地区。

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