Cargando…

Stable isotopes in the atmospheric marine boundary layer water vapour over the Atlantic Ocean, 2012–2015

The water vapour isotopic composition ((1)H(2)(16)O, H(2)(18)O and (1)H(2)H(16)O) 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 mete...

Descripción completa

Detalles Bibliográficos
Autores principales: Benetti, Marion, Steen-Larsen, Hans Christian, Reverdin, Gilles, Sveinbjörnsdóttir, Árný Erla, Aloisi, Giovanni, Berkelhammer, Max B., Bourlès, Bernard, Bourras, Denis, de Coetlogon, Gaëlle, Cosgrove, Ann, Faber, Anne-Katrine, Grelet, Jacques, Hansen, Steffen Bo, Johnson, Rod, Legoff, Hervé, Martin, Nicolas, Peters, Andrew J., Popp, Trevor James, Reynaud, Thierry, Winther, Malte
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2017
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5240618/
https://www.ncbi.nlm.nih.gov/pubmed/28094798
http://dx.doi.org/10.1038/sdata.2016.128
Descripción
Sumario:The water vapour isotopic composition ((1)H(2)(16)O, H(2)(18)O and (1)H(2)H(16)O) 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°S to 63°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.