A Song of Wind and Ice: Increased Frequency of Marine Cold-Spells in Southwestern Patagonia and Their Possible Effects on Giant Kelp Forests

dc.contributor.authorMora-Soto, Alejandra
dc.contributor.authorAguirre, C.
dc.contributor.authorIriarte, J.L.
dc.contributor.authorPalacios, M.
dc.contributor.authorMacaya, E.C.
dc.contributor.authorMacias-Fauria, M.
dc.date.accessioned2022-07-08T21:10:45Z
dc.date.available2022-07-08T21:10:45Z
dc.date.copyright2022en_US
dc.date.issued2022-06-02
dc.descriptionThe authors are deeply grateful to SHOA (Servicio Hidrográfico y Oceanográfico de la Armada de Chile) for sharing the in situ data. The authors thank Robert Schlegel and two anonymous reviewers for their thoughtful suggestions that improved the manuscript. Additionally, thanks to Maisa Rojas (CR)2 and Maycira Costa (UVIC) for their comments and Leonardo Rojas for his valuable help with R scripts.en_US
dc.description.abstractIn contrast to other coastal regions of the world, the giant kelp (Macrocystis pyrifera) ecosystem in southwestern Patagonia has been persistent in area and associated biodiversity in the last decades. In this ecoregion, sea surface temperature (SST) records have consistently remained below the upper thermal threshold for kelp survival, however, no studies have analyzed the spatiotemporal variability of SSTs and their anomalies across the geographical diversity of the southwestern Patagonian coastline. We explored the geographical distribution of extreme warm and cold events in this region from latitudes 47°–56°S in a range of ∼1,000 km, identifying the dates and spatial distribution of marine heatwaves (MHWs) and marine cold-spells (MCSs) from 1982 to 2020. Results show that a peak in the number of MHWs occurred in the great El Niño year of 1998. Additionally, the 2014–2019 period has had more severe and extreme MCSs than the previous decades. We discuss the origin of these events with a focus on three main processes: (a) geographically constrained cold events caused by glacier melting, (b) regional cold events caused by extreme winds linked to the position of the polar front, and (c) extensive SST anomalies linked to planetary-scale events such as El Niño and La Niña. Overall, those processes were conductive to counteract global warming trends locally/regionally, highlighting southwestern Patagonia as a possible climatic refugium for the giant kelp ecosystem. Despite this, the effects of freshwater inputs and storm turbulence on the exposed coasts facing the Southern Ocean may cause new kinds of stress on this ecosystem.en_US
dc.description.reviewstatusRevieweden_US
dc.description.scholarlevelFacultyen_US
dc.description.sponsorshipThis research is part of A M-S's DPhil funded by ANID-Becas Chile. CA acknowledges the support of the Agencia Nacional de Investigación y Desarrollo (ANID) Millennium Science Initiative, Program NCN19-153 and Fondecyt, Grant No. 11171163. JLI and EM were supported by FONDAP Grant Nos. 15150003, Centro de Investigación en Dinámica de Ecosistemas Marinos de Altas Latitudes (IDEAL).en_US
dc.identifier.citationMora-Soto, A., Aguirre, C., Iriarte, J. L., Palacios, M., Macaya, E. C., & Macias-Fauria, M. (2022). A song of wind and ice: Increased frequency of marine cold-spells in southwestern Patagonia and their possible effects on giant kelp forests. Journal of Geophysical Research: Oceans, 127(6), https://doi.org/10.1029/2021JC017801en_US
dc.identifier.urihttps://doi.org/10.1029/2021JC017801
dc.identifier.urihttp://hdl.handle.net/1828/14039
dc.language.isoenen_US
dc.publisherJournal of Geophysical Research: Oceansen_US
dc.subjectmarine heatwaves
dc.subjectmarine cold-spells
dc.subjectPatagonia
dc.subjectsub-Antarctic
dc.subjectgiant kelp
dc.subjectclimatic refugium
dc.subject.departmentDepartment of Geography
dc.titleA Song of Wind and Ice: Increased Frequency of Marine Cold-Spells in Southwestern Patagonia and Their Possible Effects on Giant Kelp Forestsen_US
dc.typeArticleen_US

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