Relation between the water isotopic composition in the North Atlanticmarine boundary layer and the boundary layer dynamic

Publisher's version (útgefin grein) Water isotopes are powerful tracers of the hydrological cycle and can be used to serve many purposes in climateresearch. Here, we use water isotopic measurements – in the vapour and in the precipitations – from Bermudaand Iceland measurement facilities, as we...

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Bibliographic Details
Main Authors: Sveinbjörnsdóttir, Árný, Lacour, Jean-Lionel, Steen-Larsen, Hans Christian, Peters, Andrew
Other Authors: Jarðvísindastofnun (HÍ), Institute of Earth Sciences (UI), Verkfræði- og náttúruvísindasvið (HÍ), School of Engineering and Natural Sciences (UI), Háskóli Íslands, University of Iceland
Format: Conference Object
Language:English
Published: European Geosciences Union 2019
Subjects:
Vatnafræði
Fjarkönnun
Samsætur
Veðrahvolf
Iceland
Online Access:https://hdl.handle.net/20.500.11815/2029
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Summary:Publisher's version (útgefin grein) Water isotopes are powerful tracers of the hydrological cycle and can be used to serve many purposes in climateresearch. Here, we use water isotopic measurements – in the vapour and in the precipitations – from Bermudaand Iceland measurement facilities, as well as from the Infrared Remote Sensing Interferometer (IASI), toinvestigate the feedback between evaporation and the boundary layer development through shallow convection. Icelandic Research Institute (no. 152229) Peer reviewed

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