A global analysis of the dry-dynamic forcing during cyclone growth and propagation
Mechanisms driving the intensification and propagation direction of extratropical cyclones are an active field of research. Dry-dynamic forcing factors have been established as fundamental drivers of the deepening and propagation of extratropical cyclones, but their climatological interplay, geograp...
| Published in: | Weather and Climate Dynamics |
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| Main Authors: | , , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Copernicus Publications
2021
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| Subjects: | |
| Online Access: | https://doi.org/10.5194/wcd-2-991-2021 https://doaj.org/article/2a517f03165b41a4994dcf3004c94fae |
| Summary: | Mechanisms driving the intensification and propagation direction of extratropical cyclones are an active field of research. Dry-dynamic forcing factors have been established as fundamental drivers of the deepening and propagation of extratropical cyclones, but their climatological interplay, geographical distribution, and relatedness to the observed cyclone deepening and propagation direction remain unknown. This study considers two key dry-dynamic forcing factors, the Eady growth rate (EGR) and the upper-level induced quasi-geostrophic lifting (QG ω ), and relates them to the surface deepening rates and the propagation direction during the cyclones' growth phase. To this aim, a feature-based cyclone tracking is used, and the forcing environment is climatologically analysed based on ERA-Interim data. The interplay is visualized by means of a forcing histogram, which allows one to identify different combinations of EGR and QG ω and their combined influence on the cyclone deepening (12 h sea-level pressure change) and propagation direction. The key results of the study are as follows. (i) The geographical locations of four different forcing categories, corresponding to cyclone growth in environments characterized by low QG ω and low EGR (Q ↓ E ↓ ), low QG ω but high EGR (Q ↓ E ↑ ), high QG ω and low EGR (Q ↑ E ↓ ), and high QG ω and EGR (Q ↑ E ↑ ), display distinct hot spots with only mild overlaps. For instance, cyclone growth in a Q ↑ E ↑ forcing environment is found in the entrance regions of the North Pacific and Atlantic storm tracks. Category Q ↓ E ↑ is typically found over continental North America, along the southern tip of Greenland, over parts of East Asia, and over the western North Pacific. In contrast, category Q ↑ E ↓ dominates the subtropics. (ii) The four categories are associated with different stages of the cyclones' growth phase: large EGR forcing typically occurs earlier, during the growth phase at genesis, while large QG ω forcing attains its maximum amplitude later towards maturity. (iii) ... |
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