The Connection Between North Atlantic Storm Track Regimes and Eastern Mediterranean Cyclonic Activity Article Swipe
YOU?
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· 2024
· Open Access
·
· DOI: https://doi.org/10.5194/egusphere-2024-1054
A unique chain connects the flow over the North Atlantic and the development of cyclones within the Mediterranean basin. One typical mechanism includes several successive processes: upper-level flow perturbations upstream cause Rossby wave breaking (RWB) events along the jet stream, which in turn develop into potential vorticity streamers. These streamers reach the Mediterranean, and through increased baroclinicity they enhance cyclonic activity in the region. Using ERA5 reanalysis data and rain gauge measurements, we provide a systematic analysis connecting wintertime North Atlantic storm track regimes and Eastern Mediterranean cyclones and rainfall. To do so, we use different detection algorithms for each element in the chain (RWBs, streamers and cyclones). A cluster analysis of upper tropospheric eddy kinetic energy reveals a favorable configuration of the storm track where North Atlantic storms are able to propagate farther northeast. This results in upper-level potential vorticity streamers forming more eastward alongside above-average precipitation over the Levant. Meanwhile, other latitudinal positions of the storm track (southward or northward) were found to hinder cyclonic activity in the region and reduce rainfall there. The intense rainy winter of 1991–1992 is brought as a test case to exemplify this mechanism in its extreme. We show that the rain-enhancing storm track regime was prominent throughout most of this season, alongside frequent streamers in the Eastern Mediterranean.
Related Topics
- Type
- preprint
- Language
- en
- Landing Page
- https://doi.org/10.5194/egusphere-2024-1054
- https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1054/egusphere-2024-1054.pdf
- OA Status
- gold
- Cited By
- 2
- References
- 49
- Related Works
- 10
- OpenAlex ID
- https://openalex.org/W4394691343
Raw OpenAlex JSON
- OpenAlex ID
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https://openalex.org/W4394691343Canonical identifier for this work in OpenAlex
- DOI
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https://doi.org/10.5194/egusphere-2024-1054Digital Object Identifier
- Title
-
The Connection Between North Atlantic Storm Track Regimes and Eastern Mediterranean Cyclonic ActivityWork title
- Type
-
preprintOpenAlex work type
- Language
-
enPrimary language
- Publication year
-
2024Year of publication
- Publication date
-
2024-04-10Full publication date if available
- Authors
-
Dor Sandler, Hadas Saaroni, Baruch Ziv, Talia Tamarin‐Brodsky, Nili HarnikList of authors in order
- Landing page
-
https://doi.org/10.5194/egusphere-2024-1054Publisher landing page
- PDF URL
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https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1054/egusphere-2024-1054.pdfDirect link to full text PDF
- Open access
-
YesWhether a free full text is available
- OA status
-
goldOpen access status per OpenAlex
- OA URL
-
https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1054/egusphere-2024-1054.pdfDirect OA link when available
- Concepts
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Storm track, Climatology, Baroclinity, Storm, Rossby wave, Cyclone (programming language), Geology, Atlantic hurricane, Mediterranean climate, Extratropical cyclone, Precipitation, Potential vorticity, Tropical cyclone, Oceanography, Vorticity, Meteorology, Geography, Vortex, Field-programmable gate array, Computer science, Computer hardware, ArchaeologyTop concepts (fields/topics) attached by OpenAlex
- Cited by
-
2Total citation count in OpenAlex
- Citations by year (recent)
-
2024: 2Per-year citation counts (last 5 years)
- References (count)
-
49Number of works referenced by this work
- Related works (count)
-
10Other works algorithmically related by OpenAlex
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