<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Morales MS</submitter><funding>Chilean Research Council</funding><funding>BNP Paribas | Fondation BNP Paribas</funding><funding>Consejo Nacional de Investigaciones Científicas y Técnicas</funding><funding>MINCyT | Agencia Nacional de Promoción Científica y Tecnológica</funding><funding>Russian State Assignment Project</funding><funding>Fondo Nacional de Desarrollo Cientifico, Tecnologico y de Innovacion Tecnologica, Perú</funding><funding>Inter-American Institute for Global Change Research</funding><funding>National Agency for Research and Development Chile</funding><funding>National Science Foundation</funding><pagination>16816-16823</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC7382209</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>117(29)</volume><pubmed_abstract>South American (SA) societies are highly vulnerable to droughts and pluvials, but lack of long-term climate observations severely limits our understanding of the global processes driving climatic variability in the region. The number and quality of SA climate-sensitive tree ring chronologies have significantly increased in recent decades, now providing a robust network of 286 records for characterizing hydroclimate variability since 1400 CE. We combine this network with a self-calibrated Palmer Drought Severity Index (scPDSI) dataset to derive the South American Drought Atlas (SADA) over the continent south of 12°S. The gridded annual reconstruction of austral summer scPDSI is the most spatially complete estimate of SA hydroclimate to date, and well matches past historical dry/wet events. </pubmed_abstract><journal>Proceedings of the National Academy of Sciences of the United States of America</journal><pubmed_title>Six hundred years of South American tree rings reveal an increase in severe hydroclimatic events since mid-20th century.</pubmed_title><pmcid>PMC7382209</pmcid><funding_grant_id>AGS-1602581</funding_grant_id><funding_grant_id>0148-2019-0004</funding_grant_id><funding_grant_id>ANID/PAI/77190101</funding_grant_id><funding_grant_id>ANID/FONDAP/15110009</funding_grant_id><funding_grant_id>GEO-0452325</funding_grant_id><funding_grant_id>AGS-1805490</funding_grant_id><funding_grant_id>CRN03; CRN027</funding_grant_id><funding_grant_id>PICT2013-1880</funding_grant_id><funding_grant_id>PIP11220130100584</funding_grant_id><funding_grant_id>OISE-1743738</funding_grant_id><funding_grant_id>FONDECYT-BM-INC.INV 039-2019</funding_grant_id><funding_grant_id>1161381; 1201411; 1181956 and 11161061</funding_grant_id><funding_grant_id>THEMES project</funding_grant_id><pubmed_authors>Gonzalez-Reyes A</pubmed_authors><pubmed_authors>Williams AP</pubmed_authors><pubmed_authors>Boninsegna JA</pubmed_authors><pubmed_authors>LeQuesne C</pubmed_authors><pubmed_authors>Ferrero ME</pubmed_authors><pubmed_authors>Morales MS</pubmed_authors><pubmed_authors>Bianchi LO</pubmed_authors><pubmed_authors>Flores F</pubmed_authors><pubmed_authors>Masiokas MH</pubmed_authors><pubmed_authors>Aliste D</pubmed_authors><pubmed_authors>Urrutia-Jalabert R</pubmed_authors><pubmed_authors>Lopez L</pubmed_authors><pubmed_authors>Couvreux F</pubmed_authors><pubmed_authors>Matskovsky V</pubmed_authors><pubmed_authors>Lister D</pubmed_authors><pubmed_authors>Lara A</pubmed_authors><pubmed_authors>Aguilera-Betti I</pubmed_authors><pubmed_authors>Smerdon JE</pubmed_authors><pubmed_authors>Velazquez G</pubmed_authors><pubmed_authors>Cook ER</pubmed_authors><pubmed_authors>Christie DA</pubmed_authors><pubmed_authors>Rodriguez-Caton M</pubmed_authors><pubmed_authors>Srur AM</pubmed_authors><pubmed_authors>Aravena JC</pubmed_authors><pubmed_authors>Rojas-Badilla M</pubmed_authors><pubmed_authors>Cuq E</pubmed_authors><pubmed_authors>Rojas F</pubmed_authors><pubmed_authors>Prieto MR</pubmed_authors><pubmed_authors>Villalba R</pubmed_authors><pubmed_authors>Munoz T</pubmed_authors><pubmed_authors>Alvarez C</pubmed_authors><pubmed_authors>Barichivich J</pubmed_authors><pubmed_authors>Luckman BH</pubmed_authors><pubmed_authors>Marcotti E</pubmed_authors><pubmed_authors>Munoz AA</pubmed_authors><pubmed_authors>Mundo IA</pubmed_authors><pubmed_authors>Harris I</pubmed_authors><pubmed_authors>Jones PD</pubmed_authors></additional><is_claimable>false</is_claimable><name>Six hundred years of South American tree rings reveal an increase in severe hydroclimatic events since mid-20th century.</name><description>South American (SA) societies are highly vulnerable to droughts and pluvials, but lack of long-term climate observations severely limits our understanding of the global processes driving climatic variability in the region. The number and quality of SA climate-sensitive tree ring chronologies have significantly increased in recent decades, now providing a robust network of 286 records for characterizing hydroclimate variability since 1400 CE. We combine this network with a self-calibrated Palmer Drought Severity Index (scPDSI) dataset to derive the South American Drought Atlas (SADA) over the continent south of 12°S. The gridded annual reconstruction of austral summer scPDSI is the most spatially complete estimate of SA hydroclimate to date, and well matches past historical dry/wet events. </description><dates><release>2020-01-01T00:00:00Z</release><publication>2020 Jul</publication><modification>2025-04-05T15:19:08.053Z</modification><creation>2025-04-05T15:19:08.053Z</creation></dates><accession>S-EPMC7382209</accession><cross_references><pubmed>32632003</pubmed><doi>10.1073/pnas.2002411117</doi></cross_references></HashMap>