Tracking Atmospheric Rivers Globally: Spatial Distributions and Temporal Evolution of Life Cycle Characteristics

The Tracking Atmospheric Rivers Globally as Elongated Targets (tARget) algorithm is further developed to Version 3, adding the capability to track atmospheric river (AR) life cycles along with other refinement. The results indicate AR genesis is more frequent toward the western boundaries of midlati...

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Veröffentlicht in:Journal of geophysical research. Atmospheres 2019-12, Vol.124 (23), p.12523-12552
Hauptverfasser: Guan, Bin, Waliser, Duane E.
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Waliser, Duane E.
description The Tracking Atmospheric Rivers Globally as Elongated Targets (tARget) algorithm is further developed to Version 3, adding the capability to track atmospheric river (AR) life cycles along with other refinement. The results indicate AR genesis is more frequent toward the western boundaries of midlatitude ocean basins and nearby upstream land areas (~1 month−1) compared to the eastern boundaries (~0.5 month−1) and least frequent in tropical and polar areas (reaching toward 0). AR termination is more frequent toward the northeastern sectors of North Pacific/Atlantic and adjacent downstream land areas and in the Southern Ocean near Antarctica (~1 month−1) compared to the adjacent ocean sectors (~0.5 month−1) and least frequent in tropical areas and interior Antarctica where AR genesis is similarly infrequent. ARs tend to be longer‐lived when the genesis (termination) occurs toward the western (eastern) boundaries of midlatitude ocean basins and adjacent land areas (maximum lifetime >72 hr) compared to the opposite side of the ocean basins (24–72 hr) and when terminated at high latitudes. AR travel speed is higher in the midlatitude ocean basins and strongly steered by the zonal wind around 650 hPa. AR tracks are nearly linear in most cases, with the overall travel direction closely correlated with the direction of integrated water vapor transport (r = 0.69) although being more zonal than the latter. Temporally, ARs tend to be longer/stronger around the middle of the life cycle. Seasonal variations in AR life cycle characteristics are also examined. The handling of AR separations/mergers contributes the largest sensitivity in tracking result compared to selection/resolution of input data. Key Points A technique is introduced for spatiotemporally tracking atmospheric rivers (ARs) from genesis to termination around the globe Sensitivity of AR tracking results is examined with respect to various factors, especially, how AR separations/mergers are handled AR life cycles are quantitatively characterized, including their spatial distributions, temporal evolution, and seasonal dependence
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The results indicate AR genesis is more frequent toward the western boundaries of midlatitude ocean basins and nearby upstream land areas (~1 month−1) compared to the eastern boundaries (~0.5 month−1) and least frequent in tropical and polar areas (reaching toward 0). AR termination is more frequent toward the northeastern sectors of North Pacific/Atlantic and adjacent downstream land areas and in the Southern Ocean near Antarctica (~1 month−1) compared to the adjacent ocean sectors (~0.5 month−1) and least frequent in tropical areas and interior Antarctica where AR genesis is similarly infrequent. ARs tend to be longer‐lived when the genesis (termination) occurs toward the western (eastern) boundaries of midlatitude ocean basins and adjacent land areas (maximum lifetime &gt;72 hr) compared to the opposite side of the ocean basins (24–72 hr) and when terminated at high latitudes. AR travel speed is higher in the midlatitude ocean basins and strongly steered by the zonal wind around 650 hPa. AR tracks are nearly linear in most cases, with the overall travel direction closely correlated with the direction of integrated water vapor transport (r = 0.69) although being more zonal than the latter. Temporally, ARs tend to be longer/stronger around the middle of the life cycle. Seasonal variations in AR life cycle characteristics are also examined. The handling of AR separations/mergers contributes the largest sensitivity in tracking result compared to selection/resolution of input data. Key Points A technique is introduced for spatiotemporally tracking atmospheric rivers (ARs) from genesis to termination around the globe Sensitivity of AR tracking results is examined with respect to various factors, especially, how AR separations/mergers are handled AR life cycles are quantitatively characterized, including their spatial distributions, temporal evolution, and seasonal dependence</description><identifier>ISSN: 2169-897X</identifier><identifier>EISSN: 2169-8996</identifier><identifier>DOI: 10.1029/2019JD031205</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Algorithms ; atmospheric river ; Boundaries ; Direction ; Geophysics ; Land area ; Latitude ; Life cycle ; Life cycles ; Ocean basins ; Oceans ; reanalysis ; Seasonal variation ; Seasonal variations ; Spatial distribution ; Tracking ; Travel ; Tropical climate ; Water vapor ; Water vapor transport ; Water vapour ; Zonal winds</subject><ispartof>Journal of geophysical research. 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Atmospheres</title><description>The Tracking Atmospheric Rivers Globally as Elongated Targets (tARget) algorithm is further developed to Version 3, adding the capability to track atmospheric river (AR) life cycles along with other refinement. The results indicate AR genesis is more frequent toward the western boundaries of midlatitude ocean basins and nearby upstream land areas (~1 month−1) compared to the eastern boundaries (~0.5 month−1) and least frequent in tropical and polar areas (reaching toward 0). AR termination is more frequent toward the northeastern sectors of North Pacific/Atlantic and adjacent downstream land areas and in the Southern Ocean near Antarctica (~1 month−1) compared to the adjacent ocean sectors (~0.5 month−1) and least frequent in tropical areas and interior Antarctica where AR genesis is similarly infrequent. ARs tend to be longer‐lived when the genesis (termination) occurs toward the western (eastern) boundaries of midlatitude ocean basins and adjacent land areas (maximum lifetime &gt;72 hr) compared to the opposite side of the ocean basins (24–72 hr) and when terminated at high latitudes. AR travel speed is higher in the midlatitude ocean basins and strongly steered by the zonal wind around 650 hPa. AR tracks are nearly linear in most cases, with the overall travel direction closely correlated with the direction of integrated water vapor transport (r = 0.69) although being more zonal than the latter. Temporally, ARs tend to be longer/stronger around the middle of the life cycle. Seasonal variations in AR life cycle characteristics are also examined. The handling of AR separations/mergers contributes the largest sensitivity in tracking result compared to selection/resolution of input data. Key Points A technique is introduced for spatiotemporally tracking atmospheric rivers (ARs) from genesis to termination around the globe Sensitivity of AR tracking results is examined with respect to various factors, especially, how AR separations/mergers are handled AR life cycles are quantitatively characterized, including their spatial distributions, temporal evolution, and seasonal dependence</description><subject>Algorithms</subject><subject>atmospheric river</subject><subject>Boundaries</subject><subject>Direction</subject><subject>Geophysics</subject><subject>Land area</subject><subject>Latitude</subject><subject>Life cycle</subject><subject>Life cycles</subject><subject>Ocean basins</subject><subject>Oceans</subject><subject>reanalysis</subject><subject>Seasonal variation</subject><subject>Seasonal variations</subject><subject>Spatial distribution</subject><subject>Tracking</subject><subject>Travel</subject><subject>Tropical climate</subject><subject>Water vapor</subject><subject>Water vapor transport</subject><subject>Water vapour</subject><subject>Zonal winds</subject><issn>2169-897X</issn><issn>2169-8996</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNp9kE1LAzEQhoMoWGpv_oCAV1eTzX4k3kqr1VIQagVvSzab2NR0syZpZf-90Yp4cg7z-fDOMACcY3SFUcquU4TZfIoITlF-BAYpLlhCGSuOf_Py5RSMvN-gaBSRLM8GoFs5Lt50-wrHYWt9t5ZOC7jUe-k8nBlbc2P6G_jU8aC5gVPtg9P1LmjbesjbBq7ktrMujm731nz3oVVwoZWEk16Y6Nc8rghR1wct_Bk4Udx4OfqJQ_B8d7ua3CeLx9nDZLxIBCkJTeqGciLikYrFQ1WtClSzTKisYFmjcB3LulGEYFLkvMFlTqlkpaCEFFmOFCdDcHHQ7Zx930kfqo3duTaurFJCUsRYxlikLg-UcNZ7J1XVOb3lrq8wqr7eWv19a8TJAf_QRvb_stV8tpzmOS0o-QQWrXm2</recordid><startdate>20191216</startdate><enddate>20191216</enddate><creator>Guan, Bin</creator><creator>Waliser, Duane E.</creator><general>Blackwell Publishing Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H8D</scope><scope>H96</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L7M</scope><orcidid>https://orcid.org/0000-0003-4603-0494</orcidid><orcidid>https://orcid.org/0000-0002-8428-5984</orcidid></search><sort><creationdate>20191216</creationdate><title>Tracking Atmospheric Rivers Globally: Spatial Distributions and Temporal Evolution of Life Cycle Characteristics</title><author>Guan, Bin ; Waliser, Duane E.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3738-bd8a3c034f9345fbf60b94cf4694df1b60bbdf331365ad17588e97c8336450fa3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Algorithms</topic><topic>atmospheric river</topic><topic>Boundaries</topic><topic>Direction</topic><topic>Geophysics</topic><topic>Land area</topic><topic>Latitude</topic><topic>Life cycle</topic><topic>Life cycles</topic><topic>Ocean basins</topic><topic>Oceans</topic><topic>reanalysis</topic><topic>Seasonal variation</topic><topic>Seasonal variations</topic><topic>Spatial distribution</topic><topic>Tracking</topic><topic>Travel</topic><topic>Tropical climate</topic><topic>Water vapor</topic><topic>Water vapor transport</topic><topic>Water vapour</topic><topic>Zonal winds</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Guan, Bin</creatorcontrib><creatorcontrib>Waliser, Duane E.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Journal of geophysical research. Atmospheres</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Guan, Bin</au><au>Waliser, Duane E.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Tracking Atmospheric Rivers Globally: Spatial Distributions and Temporal Evolution of Life Cycle Characteristics</atitle><jtitle>Journal of geophysical research. Atmospheres</jtitle><date>2019-12-16</date><risdate>2019</risdate><volume>124</volume><issue>23</issue><spage>12523</spage><epage>12552</epage><pages>12523-12552</pages><issn>2169-897X</issn><eissn>2169-8996</eissn><abstract>The Tracking Atmospheric Rivers Globally as Elongated Targets (tARget) algorithm is further developed to Version 3, adding the capability to track atmospheric river (AR) life cycles along with other refinement. 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AR travel speed is higher in the midlatitude ocean basins and strongly steered by the zonal wind around 650 hPa. AR tracks are nearly linear in most cases, with the overall travel direction closely correlated with the direction of integrated water vapor transport (r = 0.69) although being more zonal than the latter. Temporally, ARs tend to be longer/stronger around the middle of the life cycle. Seasonal variations in AR life cycle characteristics are also examined. The handling of AR separations/mergers contributes the largest sensitivity in tracking result compared to selection/resolution of input data. Key Points A technique is introduced for spatiotemporally tracking atmospheric rivers (ARs) from genesis to termination around the globe Sensitivity of AR tracking results is examined with respect to various factors, especially, how AR separations/mergers are handled AR life cycles are quantitatively characterized, including their spatial distributions, temporal evolution, and seasonal dependence</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2019JD031205</doi><tpages>30</tpages><orcidid>https://orcid.org/0000-0003-4603-0494</orcidid><orcidid>https://orcid.org/0000-0002-8428-5984</orcidid></addata></record>
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subjects Algorithms
atmospheric river
Boundaries
Direction
Geophysics
Land area
Latitude
Life cycle
Life cycles
Ocean basins
Oceans
reanalysis
Seasonal variation
Seasonal variations
Spatial distribution
Tracking
Travel
Tropical climate
Water vapor
Water vapor transport
Water vapour
Zonal winds
title Tracking Atmospheric Rivers Globally: Spatial Distributions and Temporal Evolution of Life Cycle Characteristics
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