Stable isotopes in surface waters of the Atlantic Ocean: Indicators of ocean-atmosphere water fluxes and oceanic mixing processes

Author:

Benetti M.12ORCID,Reverdin G.2,Aloisi G.2,Sveinbjörnsdóttir Á.1

Affiliation:

1. Institute of Earth Sciences, University of Iceland; Reykjavik Iceland

2. LOCEAN, Sorbonne Universités, UPMC/CNRS/IRD/MNHN; Paris France

Funder

French institutions

IPSL

LOCEAN

LMD

LATMOS

LEFE/IMAGO INSU

Strasse, Strasse/SPURS, and PIRATA

OSU Ecce Terra

SO SSS

LEFE-INSU

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),Space and Planetary Science,Geochemistry and Petrology,Geophysics,Oceanography

Reference52 articles.

1. Contribution des données isotopiques de deutérium, oxygène-18, hélium-3 et tritium, à l'étude de la circulation de la Mer Rouge;Andrié;Oceanol. Acta,1989

2. Deuterium excess in marine water vapor: Dependency on relative humidity and surface wind speed during evaporation;Benetti;J. Geophys. Res. Atmos.,2014

3. Importance of boundary layer mixing for the isotopic composition of surface vapor over the subtropical North Atlantic Ocean;Benetti;J. Geophys. Res. Atmos.,2015

4. Variability of sea ice melt and meteoric water input in the surface Labrador Current off Newfoundland;Benetti;J. Geophys. Res. Oceans,2016

5. Composition of freshwater in the spring of 2014 on the southern Labrador shelf and slope;Benetti;J. Geophys. Res. Oceans,2017a

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