On the link between the North Atlantic storm track and precipitation deuterium excess in Reykjavik ...

This study establishes a robust process‐based dynamical link between the variability of the deuterium excess (d) in monthly winter precipitation in Reykjavik and the frequency of strong large‐scale ocean evaporation (SLOE) events in the subpolar North Atlantic. SLOE events are induced by cold advect...

Full description

Bibliographic Details
Main Author: Aemisegger, Franziska
Format: Article in Journal/Newspaper
Language:English
Published: ETH Zurich 2018
Subjects:
Online Access:https://dx.doi.org/10.3929/ethz-b-000311015
http://hdl.handle.net/20.500.11850/311015
id ftdatacite:10.3929/ethz-b-000311015
record_format openpolar
spelling ftdatacite:10.3929/ethz-b-000311015 2024-04-28T08:29:30+00:00 On the link between the North Atlantic storm track and precipitation deuterium excess in Reykjavik ... Aemisegger, Franziska 2018 application/pdf https://dx.doi.org/10.3929/ethz-b-000311015 http://hdl.handle.net/20.500.11850/311015 en eng ETH Zurich info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 atmospheric water cycle Extratropical cyclones precipitation moisture sources Stable water isotopes storm track dynamics strong ocean evaporation article-journal Text ScholarlyArticle Journal Article 2018 ftdatacite https://doi.org/10.3929/ethz-b-000311015 2024-04-02T12:33:25Z This study establishes a robust process‐based dynamical link between the variability of the deuterium excess (d) in monthly winter precipitation in Reykjavik and the frequency of strong large‐scale ocean evaporation (SLOE) events in the subpolar North Atlantic. SLOE events are induced by cold advection in the rear of extratropical cyclones. The link between SLOE and d emerges from the fact that a substantial fraction of moisture that precipitates in Reykjavik in winter originates from SLOE events. It is shown that positive anomalies of monthly d co‐occur with positive anomalies in the frequency of SLOE events at the moisture source of Reykjavik precipitation. An intensification and a northeastwards shift of the North Atlantic storm track acts as a driver for the enhanced SLOE frequency in months with positive anomalies in d. This link also implies that in the subpolar North Atlantic, variations of d in monthly (or seasonal) precipitation reveal information about the storm track dynamics in the vicinity of ... : Atmospheric Science Letters, 19 (12) ... Article in Journal/Newspaper North Atlantic DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic atmospheric water cycle
Extratropical cyclones
precipitation moisture sources
Stable water isotopes
storm track dynamics
strong ocean evaporation
spellingShingle atmospheric water cycle
Extratropical cyclones
precipitation moisture sources
Stable water isotopes
storm track dynamics
strong ocean evaporation
Aemisegger, Franziska
On the link between the North Atlantic storm track and precipitation deuterium excess in Reykjavik ...
topic_facet atmospheric water cycle
Extratropical cyclones
precipitation moisture sources
Stable water isotopes
storm track dynamics
strong ocean evaporation
description This study establishes a robust process‐based dynamical link between the variability of the deuterium excess (d) in monthly winter precipitation in Reykjavik and the frequency of strong large‐scale ocean evaporation (SLOE) events in the subpolar North Atlantic. SLOE events are induced by cold advection in the rear of extratropical cyclones. The link between SLOE and d emerges from the fact that a substantial fraction of moisture that precipitates in Reykjavik in winter originates from SLOE events. It is shown that positive anomalies of monthly d co‐occur with positive anomalies in the frequency of SLOE events at the moisture source of Reykjavik precipitation. An intensification and a northeastwards shift of the North Atlantic storm track acts as a driver for the enhanced SLOE frequency in months with positive anomalies in d. This link also implies that in the subpolar North Atlantic, variations of d in monthly (or seasonal) precipitation reveal information about the storm track dynamics in the vicinity of ... : Atmospheric Science Letters, 19 (12) ...
format Article in Journal/Newspaper
author Aemisegger, Franziska
author_facet Aemisegger, Franziska
author_sort Aemisegger, Franziska
title On the link between the North Atlantic storm track and precipitation deuterium excess in Reykjavik ...
title_short On the link between the North Atlantic storm track and precipitation deuterium excess in Reykjavik ...
title_full On the link between the North Atlantic storm track and precipitation deuterium excess in Reykjavik ...
title_fullStr On the link between the North Atlantic storm track and precipitation deuterium excess in Reykjavik ...
title_full_unstemmed On the link between the North Atlantic storm track and precipitation deuterium excess in Reykjavik ...
title_sort on the link between the north atlantic storm track and precipitation deuterium excess in reykjavik ...
publisher ETH Zurich
publishDate 2018
url https://dx.doi.org/10.3929/ethz-b-000311015
http://hdl.handle.net/20.500.11850/311015
genre North Atlantic
genre_facet North Atlantic
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.3929/ethz-b-000311015
_version_ 1797587683229302784