English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/195237
logo share SHARE logo core CORE   Add this article to your Mendeley library MendeleyBASE

Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL
Exportar a otros formatos:


Forty-five years of oceanographic and meteorological observations at a coastal station in the NW Mediterranean: a ground truth for satellite observations

AuthorsSalat, Jordi ; Pascual, Josep ; Flexas, María del Mar; Chin, Toshio Michael; Vazquez-Cuervo, Jorge
Mediterranean Sea
Oceanographic time series
Climate trends
Satellite ground truth
Issue DateSep-2019
CitationOcean Dynamics 69(9): 1067-1084 (2019)
AbstractMarine and atmospheric parameters, including temperature observations from surface to 80 m (at 6 depths) are measured since September 1973 on a higher-than-weekly frequency, at a coastal station 4 km offshore L’Estartit (Costa Brava; NW Mediterranean). This constitutes the longest available uninterrupted oceanographic time series in the Mediterranean Sea. The present contribution focuses on observed climatic trends in temperature (°C/year) of air (AT; 0.05), sea surface (SST; 0.03), sea at 80 m depth (S80T; 0.02) and sea level (SL; 3.1 mm/year) as well as comparison with trends estimated from coincident high-resolution satellite data. The trending evolution is not uniform across seasons, being significantly higher in spring for both AT and SST, while in autumn for S80T. Other climatological results are a stratification increase (0.02 °C/year in summer temperature difference between 20 m (S20T) and S80T), trends in summer conditions at sea (when S20T > 18 °C), estimated as 0.5 and 0.9 days/year for the starting day and period respectively, and a decreasing trend of nearly 2 days/year in the period of conditions favourable for marine evaporation (when AT < SST). This last trend may be related to the observed decrease of coastal precipitation in spring. The long-term consistency in the in situ SST measurements presents an opportunity to validate the multi-decadal trends. The good agreement for 2013–2018 (RMS 0.5–0.6, bias − 0.1 to − 0.2; trends of 0.09 °C/year in situ vs. 0.06 to 0.08 °C/year from satellite) allows considering this observational site as ground truth for satellite observations and a monitoring site for climate change
DescriptionThis article is part of the Topical Collection on the 50th International Liège Colloquium on Ocean Dynamics, Liège, Belgium, 28 May to 1 June 2018.-- 18 pages, 11 figures, 5 tables
Publisher version (URL)https://doi.org/10.1007/s10236-019-01285-z
Identifiersdoi: 10.1007/s10236-019-01285-z
issn: 1616-7341
e-issn: 1616-7228
Appears in Collections:(ICM) Artículos
Files in This Item:
File Description SizeFormat 
Salat_et_al_2019.pdf20,38 MBAdobe PDFThumbnail
Show full item record
Review this work

WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.