Carbonate system during the May 2013 MedSeA cruise

Fuente: PANGAEA
Salvato in:
Dettagli Bibliografici
Autori principali: Hassoun, Abed El Rahman, Guglielmi, Véronique, Gemayel, Elissar, Goyet, Catherine, Abboud-Abi Saab, Marie, Giani, Michele, Ziveri, Patrizia, Ingrosso, Gianmarco, Touratier, Franck
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 2015
Soggetti:
Accesso online:
Tags: Aggiungi Tag
Nessun Tag, puoi essere il primo ad aggiungerne!!
_version_ 1867168566315319296
author Hassoun, Abed El Rahman
Guglielmi, Véronique
Gemayel, Elissar
Goyet, Catherine
Abboud-Abi Saab, Marie
Giani, Michele
Ziveri, Patrizia
Ingrosso, Gianmarco
Touratier, Franck
author_facet Hassoun, Abed El Rahman
Guglielmi, Véronique
Gemayel, Elissar
Goyet, Catherine
Abboud-Abi Saab, Marie
Giani, Michele
Ziveri, Patrizia
Ingrosso, Gianmarco
Touratier, Franck
collection Datos científicos de ciencias marinas y ambientales
contents Most global ocean models are based on the assumption of a "steady state" ocean. Here, we investigate the validation of this hypothesis for the anthropized Mediterranean Sea. In order to do so, we calculated the mixing coefficients of the water masses detected in this sea via an optimum multiparameter analysis referred to as the MIX approach, using data from the BOUM (2008) and MedSeA (2013) cruises. The comparison of the mixing coefficients of each water mass, between 2008 and 2013, indicates that some of their proportions have significantly changed. Surface water mass proportions did not change significantly (Delta0.05-0.1), while intermediate and deep water mass mixing coefficients of both Eastern and Western basins were significantly modified (~Delata 0.35). This study clearly shows that the Mediterranean seawater is not in a "steady state".
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_845181
institution PANGAEA
language en
publishDate 2015
publisher PANGAEA
record_format pangaea
spellingShingle Carbonate system during the May 2013 MedSeA cruise
Hassoun, Abed El Rahman
Guglielmi, Véronique
Gemayel, Elissar
Goyet, Catherine
Abboud-Abi Saab, Marie
Giani, Michele
Ziveri, Patrizia
Ingrosso, Gianmarco
Touratier, Franck
Mediterranean Sea Acidification in a Changing Climate; MedSeA
Most global ocean models are based on the assumption of a "steady state" ocean. Here, we investigate the validation of this hypothesis for the anthropized Mediterranean Sea. In order to do so, we calculated the mixing coefficients of the water masses detected in this sea via an optimum multiparameter analysis referred to as the MIX approach, using data from the BOUM (2008) and MedSeA (2013) cruises. The comparison of the mixing coefficients of each water mass, between 2008 and 2013, indicates that some of their proportions have significantly changed. Surface water mass proportions did not change significantly (Delta0.05-0.1), while intermediate and deep water mass mixing coefficients of both Eastern and Western basins were significantly modified (~Delata 0.35). This study clearly shows that the Mediterranean seawater is not in a "steady state".
title Carbonate system during the May 2013 MedSeA cruise
topic Mediterranean Sea Acidification in a Changing Climate; MedSeA
url https://doi.org/10.1594/PANGAEA.845181