Dynamical differences between short and long blocks in the Northern Hemisphere
Blocking events are persistent weather systems that strongly impact daily weather and more importantly our societies. One reason behind their strong impact is their potential long duration, as blocking events can last from 5 days up to four-five weeks. However, the mechanisms explaining this differe...
| Main Authors: | , , , |
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| Format: | Journal article |
| Language: | English |
| Published: |
Wiley
2021
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| _version_ | 1797052861270458368 |
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| author | Drouard, M Woollings, T Sexton, DMH McSweeney, CF |
| author_facet | Drouard, M Woollings, T Sexton, DMH McSweeney, CF |
| author_sort | Drouard, M |
| collection | OXFORD |
| description | Blocking events are persistent weather systems that strongly impact daily weather and more importantly our societies. One reason behind their strong impact is their potential long duration, as blocking events can last from 5 days up to four-five weeks. However, the mechanisms explaining this difference of duration have not been properly studied yet. Here, we investigate the differences between short blocks, which last 5 days, and long blocks, which last at least 10 days. We take a broad hemispheric and annual approach to this question, while recognizing that other specific factors may play a role in particular region and seasons. We show that long blocks often involve cyclonic Rossby wave breaking, while short blocks are equally associated with cyclonic and anticyclonic wave breaking. This main result is reproduced in a coupled climate model ensemble. The lower number of long anticyclonic blocks might be due to three main reasons: One/the anticyclone is reinforced on the downstream side during anticyclonic blocks which is less conducive to persistence; two/positive synoptic eddy feedback tends to force the mean zonal wind toward a more northward position during anticyclonic blocks, whereas it forces the mean zonal wind to the south of the block during cyclonic blocks, which has been previously shown to be associated with more persistent weather patterns; three/particularly sustained eddy feedback is needed to maintain long anticyclonic blocks.
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| first_indexed | 2024-03-06T18:36:37Z |
| format | Journal article |
| id | oxford-uuid:0b7704d4-6ad5-4dd3-9f97-e78ca9d3a293 |
| institution | University of Oxford |
| language | English |
| last_indexed | 2024-03-06T18:36:37Z |
| publishDate | 2021 |
| publisher | Wiley |
| record_format | dspace |
| spelling | oxford-uuid:0b7704d4-6ad5-4dd3-9f97-e78ca9d3a2932022-03-26T09:29:38ZDynamical differences between short and long blocks in the Northern HemisphereJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:0b7704d4-6ad5-4dd3-9f97-e78ca9d3a293EnglishSymplectic ElementsWiley2021Drouard, MWoollings, TSexton, DMHMcSweeney, CFBlocking events are persistent weather systems that strongly impact daily weather and more importantly our societies. One reason behind their strong impact is their potential long duration, as blocking events can last from 5 days up to four-five weeks. However, the mechanisms explaining this difference of duration have not been properly studied yet. Here, we investigate the differences between short blocks, which last 5 days, and long blocks, which last at least 10 days. We take a broad hemispheric and annual approach to this question, while recognizing that other specific factors may play a role in particular region and seasons. We show that long blocks often involve cyclonic Rossby wave breaking, while short blocks are equally associated with cyclonic and anticyclonic wave breaking. This main result is reproduced in a coupled climate model ensemble. The lower number of long anticyclonic blocks might be due to three main reasons: One/the anticyclone is reinforced on the downstream side during anticyclonic blocks which is less conducive to persistence; two/positive synoptic eddy feedback tends to force the mean zonal wind toward a more northward position during anticyclonic blocks, whereas it forces the mean zonal wind to the south of the block during cyclonic blocks, which has been previously shown to be associated with more persistent weather patterns; three/particularly sustained eddy feedback is needed to maintain long anticyclonic blocks. |
| spellingShingle | Drouard, M Woollings, T Sexton, DMH McSweeney, CF Dynamical differences between short and long blocks in the Northern Hemisphere |
| title | Dynamical differences between short and long blocks in the Northern Hemisphere |
| title_full | Dynamical differences between short and long blocks in the Northern Hemisphere |
| title_fullStr | Dynamical differences between short and long blocks in the Northern Hemisphere |
| title_full_unstemmed | Dynamical differences between short and long blocks in the Northern Hemisphere |
| title_short | Dynamical differences between short and long blocks in the Northern Hemisphere |
| title_sort | dynamical differences between short and long blocks in the northern hemisphere |
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