@article{fdi:010068886, title = {{S}table isotopes in the atmospheric marine boundary layer water vapour over the {A}tlantic {O}cean, 2012-2015}, author = {{B}enetti, {M}. and {S}teen-{L}arsen, {H}. {C}. and {R}everdin, {G}. and {S}veinbjornsdottir, {A}. {E}. and {A}loisi, {G}. and {B}erkelhammer, {M}. {B}. and {B}ourl{\`e}s, {B}ernard and {B}ourras, {D}. and {D}e {C}oetlogon, {G}. and {C}osgrove, {A}. and {F}aber, {A}. {K}. and {G}relet, {J}acques and {H}ansen, {S}. {B}. and {J}ohnson, {R}. and {L}egoff, {H}. and {M}artin, {N}. and {P}eters, {A}. {J}. and {P}opp, {T}. {J}. and {R}eynaud, {T}. and {W}inther, {M}.}, editor = {}, language = {{ENG}}, abstract = {{T}he water vapour isotopic composition ( ({H}2{O})-{H}-1-{O}-16, ({H}2{O})-{O}-18 and ({HHO})-{H}-1-{H}-2-{O}-16) of the {A}tlantic marine boundary layer has been measured from 5 research vessels between 2012 and 2015. {U}sing laser spectroscopy analysers, measurements have been carried out continuously on samples collected 10-20 meter above sea level. {A}ll the datasets have been carefully calibrated against the international {VSMOW}-{SLAP} scale following the same protocol to build a homogeneous dataset covering the {A}tlantic {O}cean between 4 degrees {S} to 63 degrees {N}. {I}n addition, standard meteorological variables have been measured continuously, including sea surface temperatures using calibrated {T}hermo-{S}alinograph for most cruises. {A}ll calibrated observations are provided with 15-minute resolution. {W}e also provide 6-hourly data to allow easier comparisons with simulations from the isotope-enabled {G}lobal {C}irculation {M}odels. {I}n addition, backwards trajectories from the {HYSPLIT} model are supplied every 6-hours for the position of our measurements.}, keywords = {{ATLANTIQUE}}, booktitle = {}, journal = {{S}cientific {D}ata - {N}ature}, volume = {4}, numero = {}, pages = {art. 160128 [17 p.]}, ISSN = {2052-4463}, year = {2017}, DOI = {10.1038/sdata.2016.128}, URL = {https://www.documentation.ird.fr/hor/fdi:010068886}, }