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

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


Titill: Stable isotopes in the atmospheric marine boundary layer water vapour over the Atlantic Ocean, 2012–2015
Höfundur: Benetti, Marion
Steen-Larsen, Hans Christian
Reverdin, Gilles
Sveinbjörnsdóttir, Árný   orcid.org/0000-0002-0310-1283
Aloisi, Giovanni
Berkelhammer, Max B.
Bourlès, Bernard
Bourras, Denis
de Coetlogon, Gaëlle
Cosgrove, Ann
... 10 fleiri höfundar Sýna alla höfunda
Útgáfa: 2017-01-17
Tungumál: Enska
Umfang: 160128
Háskóli/Stofnun: Háskóli Íslands
University of Iceland
Svið: Verkfræði- og náttúruvísindasvið (HÍ)
School of Engineering and Natural Sciences (UI)
Deild: Jarðvísindastofnun (HÍ)
Institute of Earth Sciences (UI)
Birtist í: Scientific Data;4
ISSN: 2052-4463
DOI: 10.1038/sdata.2016.128
Efnisorð: Atmospheric science; Ocean sciences; Andrúmsloft; Haffræði
URI: https://hdl.handle.net/20.500.11815/291

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Tilvitnun:

Benetti, M. et al. Stable isotopes in the atmospheric marine boundary layer water vapour over the Atlantic Ocean, 2012–2015. Sci. Data 4:160128 doi: 10.1038/sdata.2016.128 (2017).

Útdráttur:

The water vapour isotopic composition (1H216O, H218O and 1H2H16O) 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.

Leyfi:

This work is licensed under a Creative Commons Attribution 4.0 International License. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0 Metadata associated with this Data Descriptor is available at http://www.nature.com/sdata/ and is released under the CC0 waiver to maximize reuse.

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