Preprints
https://doi.org/10.5194/egusphere-2025-1234
https://doi.org/10.5194/egusphere-2025-1234
08 Apr 2025
 | 08 Apr 2025
Status: this preprint is open for discussion and under review for Nonlinear Processes in Geophysics (NPG).

Teleconnection of Sahara to Mediterranean Basin evidenced by consecutive dust storms

Vincenzo Carbone, Vincenzo Capparelli, Jessica Castagna, Fabio Lepreti, Alfonso Senatore, and Giuseppe Mendicino

Abstract. Saharan Dust Outbreaks frequently hit the Mediterranean Basin, lasting for a few days. These phenomena have various implications for the ecosystem of the entire basin, affecting the atmosphere, lithosphere, biosphere, hydrosphere, and cryosphere. Moreover, they cause numerous hazards to human society, especially concerning the environment and health, and are particularly significant to people living in a “Dust Belt” around Sahara, including nearby areas such as the Mediterranean Basin. This study demonstrates that continuous dust intrusions from the Sahara, transported across distant geographic regions, cannot be considered random events; rather, they show long-range correlations for timescales shorter than 80 days. This behaviour generates a persistent and recurrent atmospheric pattern at inter-annual time scales and synoptic spatial scales, thus opening a new perspective for climate studies and evidencing a new kind of teleconnection between North Africa and the Mediterranean Basin.

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Vincenzo Carbone, Vincenzo Capparelli, Jessica Castagna, Fabio Lepreti, Alfonso Senatore, and Giuseppe Mendicino

Status: open (until 03 Jun 2025)

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Vincenzo Carbone, Vincenzo Capparelli, Jessica Castagna, Fabio Lepreti, Alfonso Senatore, and Giuseppe Mendicino
Vincenzo Carbone, Vincenzo Capparelli, Jessica Castagna, Fabio Lepreti, Alfonso Senatore, and Giuseppe Mendicino

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Short summary
In this work, it is shown that dust storms originating from Sahara and spreading over the Mediterranean Basin are not random events, but rather they are characterized by the presence of time correlations which extend over a timescale range up to about 80 days. The combination of statistical and atmospheric circulation analyses provides a novel and interesting picture of the atmospheric teleconnection between North Africa and the Mediterranean Basin associated with Saharan dust storms.
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