Surface temperature reconstruction using alkenones from sediment core B0406 retreived in the Peru upwelling area

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Main Authors: Gutièrrez, Dimitri, Bouloubassi, Ioanna, Sifeddine, Abdelfettah, Purca, Sara, Goubanova, Katerina, Graco, Michelle, Field, David, Méjanelle, Laurence, Velazco, Federico, Lorre, Anne, Salvatteci, Renato, Quispe, Daniel, Vargas, Gabriel, Dewitte, Boris, Ortlieb, Luc
Format: Dataset Open Access
Language:en
Published: PANGAEA 2013
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author Gutièrrez, Dimitri
Bouloubassi, Ioanna
Sifeddine, Abdelfettah
Purca, Sara
Goubanova, Katerina
Graco, Michelle
Field, David
Méjanelle, Laurence
Velazco, Federico
Lorre, Anne
Salvatteci, Renato
Quispe, Daniel
Vargas, Gabriel
Dewitte, Boris
Ortlieb, Luc
author_facet Gutièrrez, Dimitri
Bouloubassi, Ioanna
Sifeddine, Abdelfettah
Purca, Sara
Goubanova, Katerina
Graco, Michelle
Field, David
Méjanelle, Laurence
Velazco, Federico
Lorre, Anne
Salvatteci, Renato
Quispe, Daniel
Vargas, Gabriel
Dewitte, Boris
Ortlieb, Luc
collection Datos científicos de ciencias marinas y ambientales
contents We reconstructed a high-resolution, alkenone-based sea surface temperature (SST) record spanning the last ca. 150 years, from a sediment core retrieved within the main upwelling zone off Peru. A conspicuous SST decline is evidenced since the 1950s despite interdecadal SST variability. Instrumental SST data and reanalysis of ECMWF ERA 40 winds suggest that the recent coastal cooling corresponds mainly to an intensification of alongshore winds and associated increase of upwelling in spring. Consistently, both proxy and instrumental data evidence increased productivity in phase with the SST cooling. Our data expand on previous reports on recent SST cooling in other Eastern Boundary upwelling systems and support scenarios that relate coastal upwelling intensification to global warming. Yet, further investigations are needed to assess the role of different mechanisms and forcings (enhanced local winds vs. spin-up of the South Pacific High Pressure cell).
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_808961
institution PANGAEA
language en
publishDate 2013
publisher PANGAEA
record_format pangaea
spellingShingle Surface temperature reconstruction using alkenones from sediment core B0406 retreived in the Peru upwelling area
Gutièrrez, Dimitri
Bouloubassi, Ioanna
Sifeddine, Abdelfettah
Purca, Sara
Goubanova, Katerina
Graco, Michelle
Field, David
Méjanelle, Laurence
Velazco, Federico
Lorre, Anne
Salvatteci, Renato
Quispe, Daniel
Vargas, Gabriel
Dewitte, Boris
Ortlieb, Luc
Age; AGE; Alkenone, unsaturation index UK'37; B0406; Calculated from C37 alkenones (Prahl & Wakeham, 1987); DEPTH, sediment/rock; GC; Gravity corer; Sea surface temperature; World Ocean
We reconstructed a high-resolution, alkenone-based sea surface temperature (SST) record spanning the last ca. 150 years, from a sediment core retrieved within the main upwelling zone off Peru. A conspicuous SST decline is evidenced since the 1950s despite interdecadal SST variability. Instrumental SST data and reanalysis of ECMWF ERA 40 winds suggest that the recent coastal cooling corresponds mainly to an intensification of alongshore winds and associated increase of upwelling in spring. Consistently, both proxy and instrumental data evidence increased productivity in phase with the SST cooling. Our data expand on previous reports on recent SST cooling in other Eastern Boundary upwelling systems and support scenarios that relate coastal upwelling intensification to global warming. Yet, further investigations are needed to assess the role of different mechanisms and forcings (enhanced local winds vs. spin-up of the South Pacific High Pressure cell).
title Surface temperature reconstruction using alkenones from sediment core B0406 retreived in the Peru upwelling area
topic Age; AGE; Alkenone, unsaturation index UK'37; B0406; Calculated from C37 alkenones (Prahl & Wakeham, 1987); DEPTH, sediment/rock; GC; Gravity corer; Sea surface temperature; World Ocean
url https://doi.org/10.1594/PANGAEA.808961