Initiation of a stable convective hydroclimatic regime in Central America circa 9000 years BP

What drives hydroclimate changes in tropical regions is not well known. Here, the authors present a 12,000 year long precipitation record from Guetemala which shows that exceeding a threshold in sea surface temperatures caused Central American rainfall to change from a dry to an active convective re...

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Autores principales:	Amos Winter, Davide Zanchettin, Matthew Lachniet, Rolf Vieten, Francesco S. R. Pausata, Fredrik Charpentier Ljungqvist, Hai Cheng, R. Lawrence Edwards, Thomas Miller, Sara Rubinetti, Angelo Rubino, Carla Taricco
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2020
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/1a87d0dee8664cbbaf0696d91db59d66
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spelling	oai:doaj.org-article:1a87d0dee8664cbbaf0696d91db59d662021-12-02T17:31:54ZInitiation of a stable convective hydroclimatic regime in Central America circa 9000 years BP10.1038/s41467-020-14490-y2041-1723https://doaj.org/article/1a87d0dee8664cbbaf0696d91db59d662020-02-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-14490-yhttps://doaj.org/toc/2041-1723What drives hydroclimate changes in tropical regions is not well known. Here, the authors present a 12,000 year long precipitation record from Guetemala which shows that exceeding a threshold in sea surface temperatures caused Central American rainfall to change from a dry to an active convective regime around 9000 years ago.Amos WinterDavide ZanchettinMatthew LachnietRolf VietenFrancesco S. R. PausataFredrik Charpentier LjungqvistHai ChengR. Lawrence EdwardsThomas MillerSara RubinettiAngelo RubinoCarla TariccoNature PortfolioarticleScienceQENNature Communications, Vol 11, Iss 1, Pp 1-8 (2020)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Amos Winter Davide Zanchettin Matthew Lachniet Rolf Vieten Francesco S. R. Pausata Fredrik Charpentier Ljungqvist Hai Cheng R. Lawrence Edwards Thomas Miller Sara Rubinetti Angelo Rubino Carla Taricco Initiation of a stable convective hydroclimatic regime in Central America circa 9000 years BP
description	What drives hydroclimate changes in tropical regions is not well known. Here, the authors present a 12,000 year long precipitation record from Guetemala which shows that exceeding a threshold in sea surface temperatures caused Central American rainfall to change from a dry to an active convective regime around 9000 years ago.
format	article
author	Amos Winter Davide Zanchettin Matthew Lachniet Rolf Vieten Francesco S. R. Pausata Fredrik Charpentier Ljungqvist Hai Cheng R. Lawrence Edwards Thomas Miller Sara Rubinetti Angelo Rubino Carla Taricco
author_facet	Amos Winter Davide Zanchettin Matthew Lachniet Rolf Vieten Francesco S. R. Pausata Fredrik Charpentier Ljungqvist Hai Cheng R. Lawrence Edwards Thomas Miller Sara Rubinetti Angelo Rubino Carla Taricco
author_sort	Amos Winter
title	Initiation of a stable convective hydroclimatic regime in Central America circa 9000 years BP
title_short	Initiation of a stable convective hydroclimatic regime in Central America circa 9000 years BP
title_full	Initiation of a stable convective hydroclimatic regime in Central America circa 9000 years BP
title_fullStr	Initiation of a stable convective hydroclimatic regime in Central America circa 9000 years BP
title_full_unstemmed	Initiation of a stable convective hydroclimatic regime in Central America circa 9000 years BP
title_sort	initiation of a stable convective hydroclimatic regime in central america circa 9000 years bp
publisher	Nature Portfolio
publishDate	2020
url	https://doaj.org/article/1a87d0dee8664cbbaf0696d91db59d66
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Initiation of a stable convective hydroclimatic regime in Central America circa 9000 years BP

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