Publications des scientifiques de l'IRD

Benetti M., Steen-Larsen H. C., Reverdin G., Sveinbjornsdottir A. E., Aloisi G., Berkelhammer M. B., Bourlès Bernard, Bourras D., De Coetlogon G., Cosgrove A., Faber A. K., Grelet Jacques, Hansen S. B., Johnson R., Legoff H., Martin N., Peters A. J., Popp T. J., Reynaud T., Winther M. (2017). Stable isotopes in the atmospheric marine boundary layer water vapour over the Atlantic Ocean, 2012-2015. Scientific Data - Nature, 4, p. art. 160128 [17 p.]. ISSN 2052-4463.

Titre du document
Stable isotopes in the atmospheric marine boundary layer water vapour over the Atlantic Ocean, 2012-2015
Année de publication
2017
Type de document
Article référencé dans le Web of Science WOS:000392065000002
Auteurs
Benetti M., Steen-Larsen H. C., Reverdin G., Sveinbjornsdottir A. E., Aloisi G., Berkelhammer M. B., Bourlès Bernard, Bourras D., De Coetlogon G., Cosgrove A., Faber A. K., Grelet Jacques, Hansen S. B., Johnson R., Legoff H., Martin N., Peters A. J., Popp T. J., Reynaud T., Winther M.
Source
Scientific Data - Nature, 2017, 4, p. art. 160128 [17 p.] ISSN 2052-4463
The water vapour isotopic composition ( (H2O)-H-1-O-16, (H2O)-O-18 and (HHO)-H-1-H-2-O-16) of the Atlantic marine boundary layer has been measured from 5 research vessels between 2012 and 2015. Using laser spectroscopy analysers, measurements have been carried out continuously on samples collected 10-20 meter above sea level. All the datasets have been carefully calibrated against the international VSMOW-SLAP scale following the same protocol to build a homogeneous dataset covering the Atlantic Ocean between 4 degrees S to 63 degrees N. In addition, standard meteorological variables have been measured continuously, including sea surface temperatures using calibrated Thermo-Salinograph for most cruises. All calibrated observations are provided with 15-minute resolution. We also provide 6-hourly data to allow easier comparisons with simulations from the isotope-enabled Global Circulation Models. In addition, backwards trajectories from the HYSPLIT model are supplied every 6-hours for the position of our measurements.
Plan de classement
Limnologie physique / Océanographie physique [032]
Description Géographique
ATLANTIQUE
Localisation
Fonds IRD [F B010068886]
Identifiant IRD
fdi:010068886
Contact