Structure and evolution of intense austral cut‐off lows
This study examines the three‐dimensional structure and evolution of the 200 most intense Cut‐off Lows (COLs) in the Southern Hemisphere (SH). This is done using feature tracking and cyclone‐centred compositing based on the ERA‐Interim reanalysis. Composites confirm the existence of a well‐defined t...
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Veröffentlicht in: | Quarterly journal of the Royal Meteorological Society 2021-01, Vol.147 (734), p.1-20 |
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description | This study examines the three‐dimensional structure and evolution of the 200 most intense Cut‐off Lows (COLs) in the Southern Hemisphere (SH). This is done using feature tracking and cyclone‐centred compositing based on the ERA‐Interim reanalysis. Composites confirm the existence of a well‐defined tropospheric moist cold core co‐located with warm dry air in the lower stratosphere. Such cores are surrounded by regions of strong temperature gradients (frontal zones) which move downstream throughout the life cycle. The stratospheric air intrusion into the troposphere is identified in vertical cross‐sections of potential vorticity and ozone, a process referred to as tropopause folding. Precipitation occurs ahead of the COLs because of the low (high)‐level convergence (divergence) and strong upward motion. The maximum precipitation is observed during decay, indicating a possible link between COLs and surface cyclones. Composites conditioned on relative vorticity and precipitable water suggest these variables may be related to precipitation. The COLs exhibit a westward tilt during their early stages but they change to a barotropic state in the mature stage. Finally, the main characteristics of the COLs are summarised by categories which discriminate different intensities, indicating there are differences in the structure of COLs with consequences for precipitation. These efforts aim to provide new insights into the development of COLs in the SH which could aid in identifying and forecasting their various types and associated precipitation patterns.
The understanding of the structure and life cycle of Cut‐off Lows is one of the keys to understand their associated cloud and precipitation features. Motivated by the limited number of studies on the structure of Cut‐off Lows, this study provides the first robust view of the structure, evolution and properties of intense austral Cut‐off Lows including how their precipitation depends on their structure. This study may serve as a reference guide for the diagnosis of Cut‐off Lows, helping meteorologists to better understand weather patterns and produce better forecasts. |
doi_str_mv | 10.1002/qj.3900 |
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The understanding of the structure and life cycle of Cut‐off Lows is one of the keys to understand their associated cloud and precipitation features. Motivated by the limited number of studies on the structure of Cut‐off Lows, this study provides the first robust view of the structure, evolution and properties of intense austral Cut‐off Lows including how their precipitation depends on their structure. This study may serve as a reference guide for the diagnosis of Cut‐off Lows, helping meteorologists to better understand weather patterns and produce better forecasts.</description><identifier>ISSN: 0035-9009</identifier><identifier>EISSN: 1477-870X</identifier><identifier>DOI: 10.1002/qj.3900</identifier><language>eng</language><publisher>Chichester, UK: John Wiley & Sons, Ltd</publisher><subject>Barotropic mode ; composites ; cut‐off lows ; Cyclones ; Divergence ; Dry air ; Evolution ; Frontal zones ; Life cycle ; Life cycles ; Lower stratosphere ; Maximum precipitation ; Ozone ; Potential vorticity ; Precipitable water ; Precipitation ; Precipitation patterns ; Relative vorticity ; Southern Hemisphere ; Stratosphere ; structure ; Temperature gradients ; Tropopause ; Troposphere</subject><ispartof>Quarterly journal of the Royal Meteorological Society, 2021-01, Vol.147 (734), p.1-20</ispartof><rights>2020 Royal Meteorological Society</rights><rights>2021 Royal Meteorological Society</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3220-a02133cff92557bb642734fc67a79c26392c0d7c2c74c7aac1ca808007b38db3</citedby><cites>FETCH-LOGICAL-c3220-a02133cff92557bb642734fc67a79c26392c0d7c2c74c7aac1ca808007b38db3</cites><orcidid>0000-0003-4363-3206</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2Fqj.3900$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2Fqj.3900$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1417,27924,27925,45574,45575</link.rule.ids></links><search><creatorcontrib>Pinheiro, Henri</creatorcontrib><creatorcontrib>Gan, Manoel</creatorcontrib><creatorcontrib>Hodges, Kevin</creatorcontrib><title>Structure and evolution of intense austral cut‐off lows</title><title>Quarterly journal of the Royal Meteorological Society</title><description>This study examines the three‐dimensional structure and evolution of the 200 most intense Cut‐off Lows (COLs) in the Southern Hemisphere (SH). This is done using feature tracking and cyclone‐centred compositing based on the ERA‐Interim reanalysis. Composites confirm the existence of a well‐defined tropospheric moist cold core co‐located with warm dry air in the lower stratosphere. Such cores are surrounded by regions of strong temperature gradients (frontal zones) which move downstream throughout the life cycle. The stratospheric air intrusion into the troposphere is identified in vertical cross‐sections of potential vorticity and ozone, a process referred to as tropopause folding. Precipitation occurs ahead of the COLs because of the low (high)‐level convergence (divergence) and strong upward motion. The maximum precipitation is observed during decay, indicating a possible link between COLs and surface cyclones. Composites conditioned on relative vorticity and precipitable water suggest these variables may be related to precipitation. The COLs exhibit a westward tilt during their early stages but they change to a barotropic state in the mature stage. Finally, the main characteristics of the COLs are summarised by categories which discriminate different intensities, indicating there are differences in the structure of COLs with consequences for precipitation. These efforts aim to provide new insights into the development of COLs in the SH which could aid in identifying and forecasting their various types and associated precipitation patterns.
The understanding of the structure and life cycle of Cut‐off Lows is one of the keys to understand their associated cloud and precipitation features. Motivated by the limited number of studies on the structure of Cut‐off Lows, this study provides the first robust view of the structure, evolution and properties of intense austral Cut‐off Lows including how their precipitation depends on their structure. This study may serve as a reference guide for the diagnosis of Cut‐off Lows, helping meteorologists to better understand weather patterns and produce better forecasts.</description><subject>Barotropic mode</subject><subject>composites</subject><subject>cut‐off lows</subject><subject>Cyclones</subject><subject>Divergence</subject><subject>Dry air</subject><subject>Evolution</subject><subject>Frontal zones</subject><subject>Life cycle</subject><subject>Life cycles</subject><subject>Lower stratosphere</subject><subject>Maximum precipitation</subject><subject>Ozone</subject><subject>Potential vorticity</subject><subject>Precipitable water</subject><subject>Precipitation</subject><subject>Precipitation patterns</subject><subject>Relative vorticity</subject><subject>Southern Hemisphere</subject><subject>Stratosphere</subject><subject>structure</subject><subject>Temperature gradients</subject><subject>Tropopause</subject><subject>Troposphere</subject><issn>0035-9009</issn><issn>1477-870X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNp10M1Kw0AQB_BFFIxVfIWABw-SOtlNOtmjFD8piNiDt2Wz3YWEmG33w9Kbj-Az-iSmxqungZkf_4E_Iec5THMAer1pp4wDHJAkLxCzCuHtkCQArMyGNT8mJ963AFAixYTw1-CiCtHpVParVH_YLobG9qk1adMH3fvhEH1wsktVDN-fX9aYtLNbf0qOjOy8PvubE7K8u13OH7LF8_3j_GaRKUYpZBJozpgyhtOyxLqeFRRZYdQMJXJFZ4xTBStUVGGhUEqVK1lBBYA1q1Y1m5CLMXbt7CZqH0Rro-uHj4IWVQlYckYHdTkq5az3Thuxds27dDuRg9jXIjat2NcyyKtRbptO7_5j4uXpV_8AzC5iYQ</recordid><startdate>202101</startdate><enddate>202101</enddate><creator>Pinheiro, Henri</creator><creator>Gan, Manoel</creator><creator>Hodges, Kevin</creator><general>John Wiley & Sons, Ltd</general><general>Wiley Subscription Services, Inc</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><orcidid>https://orcid.org/0000-0003-4363-3206</orcidid></search><sort><creationdate>202101</creationdate><title>Structure and evolution of intense austral cut‐off lows</title><author>Pinheiro, Henri ; Gan, Manoel ; Hodges, Kevin</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3220-a02133cff92557bb642734fc67a79c26392c0d7c2c74c7aac1ca808007b38db3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Barotropic mode</topic><topic>composites</topic><topic>cut‐off lows</topic><topic>Cyclones</topic><topic>Divergence</topic><topic>Dry air</topic><topic>Evolution</topic><topic>Frontal zones</topic><topic>Life cycle</topic><topic>Life cycles</topic><topic>Lower stratosphere</topic><topic>Maximum precipitation</topic><topic>Ozone</topic><topic>Potential vorticity</topic><topic>Precipitable water</topic><topic>Precipitation</topic><topic>Precipitation patterns</topic><topic>Relative vorticity</topic><topic>Southern Hemisphere</topic><topic>Stratosphere</topic><topic>structure</topic><topic>Temperature gradients</topic><topic>Tropopause</topic><topic>Troposphere</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Pinheiro, Henri</creatorcontrib><creatorcontrib>Gan, Manoel</creatorcontrib><creatorcontrib>Hodges, Kevin</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Quarterly journal of the Royal Meteorological Society</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Pinheiro, Henri</au><au>Gan, Manoel</au><au>Hodges, Kevin</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Structure and evolution of intense austral cut‐off lows</atitle><jtitle>Quarterly journal of the Royal Meteorological Society</jtitle><date>2021-01</date><risdate>2021</risdate><volume>147</volume><issue>734</issue><spage>1</spage><epage>20</epage><pages>1-20</pages><issn>0035-9009</issn><eissn>1477-870X</eissn><abstract>This study examines the three‐dimensional structure and evolution of the 200 most intense Cut‐off Lows (COLs) in the Southern Hemisphere (SH). This is done using feature tracking and cyclone‐centred compositing based on the ERA‐Interim reanalysis. Composites confirm the existence of a well‐defined tropospheric moist cold core co‐located with warm dry air in the lower stratosphere. Such cores are surrounded by regions of strong temperature gradients (frontal zones) which move downstream throughout the life cycle. The stratospheric air intrusion into the troposphere is identified in vertical cross‐sections of potential vorticity and ozone, a process referred to as tropopause folding. Precipitation occurs ahead of the COLs because of the low (high)‐level convergence (divergence) and strong upward motion. The maximum precipitation is observed during decay, indicating a possible link between COLs and surface cyclones. Composites conditioned on relative vorticity and precipitable water suggest these variables may be related to precipitation. The COLs exhibit a westward tilt during their early stages but they change to a barotropic state in the mature stage. Finally, the main characteristics of the COLs are summarised by categories which discriminate different intensities, indicating there are differences in the structure of COLs with consequences for precipitation. These efforts aim to provide new insights into the development of COLs in the SH which could aid in identifying and forecasting their various types and associated precipitation patterns.
The understanding of the structure and life cycle of Cut‐off Lows is one of the keys to understand their associated cloud and precipitation features. Motivated by the limited number of studies on the structure of Cut‐off Lows, this study provides the first robust view of the structure, evolution and properties of intense austral Cut‐off Lows including how their precipitation depends on their structure. This study may serve as a reference guide for the diagnosis of Cut‐off Lows, helping meteorologists to better understand weather patterns and produce better forecasts.</abstract><cop>Chichester, UK</cop><pub>John Wiley & Sons, Ltd</pub><doi>10.1002/qj.3900</doi><tpages>21</tpages><orcidid>https://orcid.org/0000-0003-4363-3206</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Barotropic mode composites cut‐off lows Cyclones Divergence Dry air Evolution Frontal zones Life cycle Life cycles Lower stratosphere Maximum precipitation Ozone Potential vorticity Precipitable water Precipitation Precipitation patterns Relative vorticity Southern Hemisphere Stratosphere structure Temperature gradients Tropopause Troposphere |
title | Structure and evolution of intense austral cut‐off lows |
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