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Vb Cyclones Synchronized With the Arctic-/North Atlantic Oscillation.
M Hofstätter1,2, G Blöschl3
1Department of Climate Research Central Institute for Meteorology and Geodynamics Vienna Austria.
Vb cyclones, originating in the Western Mediterranean, show non-random occurrence patterns with distinct clusters and hiatus periods. Their frequency is linked to atmospheric circulation and climate oscillations like the North Atlantic Oscillation.
Area of Science:
- Meteorology and Climatology
- Atmospheric Science
- Ocean-Atmosphere Interactions
Background:
- Vb cyclones are significant weather phenomena originating in the Western Mediterranean, impacting Central Europe.
- Understanding their temporal occurrence is crucial for climate and weather forecasting.
- Previous studies have highlighted their impact but lacked detailed temporal analysis.
Purpose of the Study:
- To investigate the temporal characteristics and occurrence patterns of Vb cyclones.
- To identify clustering and hiatus periods in Vb cyclone activity.
- To explore the relationship between Vb cyclone occurrence and large-scale atmospheric circulation patterns, including the Northern Atlantic Oscillation (NAO) and Arctic Oscillation (AO).
Main Methods:
- Analysis of Vb cyclone tracks at Z700 and sea level pressure using JRA-55 reanalysis data (1959-2015).
- Identification of distinct clusters and hiatus periods in cyclone occurrence.
- Correlation analysis with atmospheric circulation indices (NAO and AO) at different pressure levels.
Main Results:
- Vb cyclone risk was highest in the 1960s, decreasing thereafter.
- Cyclone occurrences are not random, exhibiting 11 distinct clusters and 11 hiatus periods.
- Clustering is particularly evident for Genoan cyclones in summer and those near the Iberian Peninsula/North African coast in winter.
- Superposition of polar and subtropical jet streams over the Western Mediterranean is a key feature at Vb onset.
- Vb cyclone occurrence is synchronized with negative phases of NAO and AO, with reduced frequency during positive phases.
Conclusions:
- Vb cyclone activity exhibits significant temporal variability and non-random clustering.
- Large-scale atmospheric circulation, particularly jet stream configuration and phases of NAO/AO, strongly influences Vb cyclone occurrence.
- The findings provide insights into the predictability and behavior of these impactful weather systems.
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