Variability of Iberian upwelling implied by ERA-40 and ERA-Interim reanalyses

The Regional Ocean Modeling System ocean model is used to simulate the decadal evolution of the regional waters in offshore Iberia in response to atmospheric fields given by ECMWF ERA-40 (1961–2001) and ERA-Interim (1989–2008) reanalyses. The simulated sea surface temperature (...

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Main Authors: José M. R. Alves, Pedro M. A. Miranda
Format: Article
Language:English
Published: Stockholm University Press 2013-05-01
Series:Tellus: Series A, Dynamic Meteorology and Oceanography
Subjects:
Online Access:http://www.tellusa.net/index.php/tellusa/article/download/19245/pdf_1
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author José M. R. Alves
Pedro M. A. Miranda
author_facet José M. R. Alves
Pedro M. A. Miranda
author_sort José M. R. Alves
collection DOAJ
description The Regional Ocean Modeling System ocean model is used to simulate the decadal evolution of the regional waters in offshore Iberia in response to atmospheric fields given by ECMWF ERA-40 (1961–2001) and ERA-Interim (1989–2008) reanalyses. The simulated sea surface temperature (SST) fields are verified against satellite AVHRR SST, and they are analysed to characterise the variability and trends of coastal upwelling in the region. Opposing trends in upwelling frequency are found at the northern limit, where upwelling has been decreasing in recent decades, and at its southern edge, where there is some evidence of increased upwelling. These results confirm previous observational studies and, more importantly, indicate that observed SST trends are not only due to changes in radiative or atmospheric heat fluxes alone but also due to changes in upwelling dynamics, suggesting that such a process may be relevant in climate change scenarios.
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spelling doaj.art-0358101cdbbe4cf5be1126d9b16c7a1e2022-12-21T22:51:04ZengStockholm University PressTellus: Series A, Dynamic Meteorology and Oceanography0280-64951600-08702013-05-0165011210.3402/tellusa.v65i0.19245Variability of Iberian upwelling implied by ERA-40 and ERA-Interim reanalysesJosé M. R. AlvesPedro M. A. MirandaThe Regional Ocean Modeling System ocean model is used to simulate the decadal evolution of the regional waters in offshore Iberia in response to atmospheric fields given by ECMWF ERA-40 (1961–2001) and ERA-Interim (1989–2008) reanalyses. The simulated sea surface temperature (SST) fields are verified against satellite AVHRR SST, and they are analysed to characterise the variability and trends of coastal upwelling in the region. Opposing trends in upwelling frequency are found at the northern limit, where upwelling has been decreasing in recent decades, and at its southern edge, where there is some evidence of increased upwelling. These results confirm previous observational studies and, more importantly, indicate that observed SST trends are not only due to changes in radiative or atmospheric heat fluxes alone but also due to changes in upwelling dynamics, suggesting that such a process may be relevant in climate change scenarios.http://www.tellusa.net/index.php/tellusa/article/download/19245/pdf_1climate changeupwellingROMSreanalyses
spellingShingle José M. R. Alves
Pedro M. A. Miranda
Variability of Iberian upwelling implied by ERA-40 and ERA-Interim reanalyses
Tellus: Series A, Dynamic Meteorology and Oceanography
climate change
upwelling
ROMS
reanalyses
title Variability of Iberian upwelling implied by ERA-40 and ERA-Interim reanalyses
title_full Variability of Iberian upwelling implied by ERA-40 and ERA-Interim reanalyses
title_fullStr Variability of Iberian upwelling implied by ERA-40 and ERA-Interim reanalyses
title_full_unstemmed Variability of Iberian upwelling implied by ERA-40 and ERA-Interim reanalyses
title_short Variability of Iberian upwelling implied by ERA-40 and ERA-Interim reanalyses
title_sort variability of iberian upwelling implied by era 40 and era interim reanalyses
topic climate change
upwelling
ROMS
reanalyses
url http://www.tellusa.net/index.php/tellusa/article/download/19245/pdf_1
work_keys_str_mv AT josx00e9mralves variabilityofiberianupwellingimpliedbyera40anderainterimreanalyses
AT pedromamiranda variabilityofiberianupwellingimpliedbyera40anderainterimreanalyses