@article{fdi:010061957, title = {{D}euterium excess in marine water vapor : dependency on relative humidity and surface wind speed during evaporation}, author = {{B}enetti, {M}. and {R}everdin, {G}. and {P}ierre, {C}. and {M}erlivat, {L}. and {R}isi, {C}. and {S}teen-{L}arsen, {H}. {C}. and {V}imeux, {F}ran{\c{c}}oise}, editor = {}, language = {{ENG}}, abstract = {{W}e provide the first continuous measurements of isotopic composition ({D} and {O}-18) of water vapor over the subtropical {E}astern {N}orth {A}tlantic {O}cean from mid-{A}ugust to mid-{S}eptember 2012. {T}he ship was located mostly around 26 degrees {N}, 35 degrees {W} where evaporation exceeded by far precipitation and water vapor at 20m largely originated from surface evaporation. {T}he only large deviations from that occurred during a 2 day period in the vicinity of a weak low-pressure system. {T}he continuous measurements were used to investigate deuterium excess (d-excess) relation to evaporation. {D}uring 25 days d-excess was negatively correlated with relative humidity (r(2)=0.89). {M}oreover, d-excess estimated in an evaporative model with a closure assumption reproduced most of the observed variability. {F}rom these observations, the d-excess parameter seems to be a good indicator of evaporative conditions. {W}e also conclude that in this region, d-excess into the marine boundary layer is less affected by mixing with the free troposphere than the isotopic composition. {F}rom our data, the transition from smooth to rough regime at the ocean surface is associated with a d-excess decrease of 5, which suggests the importance of the ocean surface roughness in controlling d-excess in this region.}, keywords = {{D}euterium excess ; evaporation ; wind speed ; surface roughness ; {ATLANTIQUE} {NORD} {EST}}, booktitle = {}, journal = {{J}ournal of {G}eophysical {R}esearch.{A}tmospheres}, volume = {119}, numero = {2}, pages = {584--593}, ISSN = {2169-897{X}}, year = {2014}, DOI = {10.1002/2013jd020535}, URL = {https://www.documentation.ird.fr/hor/fdi:010061957}, }