Preprints
https://doi.org/10.5194/egusphere-2024-2978
https://doi.org/10.5194/egusphere-2024-2978
26 Sep 2024
 | 26 Sep 2024
Status: this preprint is open for discussion and under review for Weather and Climate Dynamics (WCD).

Environments and lifting mechanisms of cold-frontal convective cells during the warm-season in Germany

George Pacey, Stephan Pfahl, and Lisa Schielicke

Abstract.

Convection often initiates in proximity to cold fronts during the warm-season, but how various processes favour convective initiation at different regions relative to the front is still not well-understood. By combining automatic front detection methods and a convective cell tracking and detection dataset, the environments and availability of different lifting mechanisms are analysed. Our results indicate that pre-surface-frontal cells form in the environments with the highest surface dew points and convective available potential instability (CAPE). At other front relative regions, cells form in environments with lower CAPE and surface dew points, though still significantly higher than regions without cells. Mid-level relative humidity discriminates particularly well between post-frontal cell locations and regions without cells. Pre-surface-frontal cells form in environments with the strongest large-scale lifting at 850 hPa and 700 hPa and also with the strongest convective inhibition. We also observe importance of large-scale lifting post-frontal, particularly at 500 hPa. Observational sunshine duration data indicate less sunshine before cell initiation compared to regions without cells at most front relative regions, which highlights that solar heating may not be responsible for the majority of cold-frontal cell initiation. The results in this study are an important step towards a deeper understanding of the drivers of cold-frontal convection at different regions relative to the front.

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George Pacey, Stephan Pfahl, and Lisa Schielicke

Status: open (until 07 Nov 2024)

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George Pacey, Stephan Pfahl, and Lisa Schielicke
George Pacey, Stephan Pfahl, and Lisa Schielicke

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Short summary
Cold fronts are often associated with areas of intense precipitation (cells) in the warm-season, but the drivers and environments of cells at different locations relative to the front are not well-understood. We show that cells ahead of the surface front have the highest amount of environmental instability and moisture. Also, low-level lifting is maximised ahead of the surface front and upper-level lifting is particularly important for cell initiation behind the front.