Polarimetric Radar Observations from a Waterspout-Producing Thunderstorm
A family of four waterspouts was produced by a convective cell over western Lake Michigan on 12 September 2013. This storm initiated along a boundary north of a mesolow in a low-level cold-air advection regime, and developed supercell characteristics once the second waterspout was in progress. Polar...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Matthew S Van Den Broeke [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Weather and forecasting - Boston, Mass. : AMS, 1986, 30(2015), 2, Seite 329-348 |
|---|---|
| Übergeordnetes Werk: |
volume:30 ; year:2015 ; number:2 ; pages:329-348 |
| Links: |
|---|
| DOI / URN: |
10.1175/WAF-D-14-00114.1 |
|---|
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OLC1957752408 |
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| 520 | |a A family of four waterspouts was produced by a convective cell over western Lake Michigan on 12 September 2013. This storm initiated along a boundary north of a mesolow in a low-level cold-air advection regime, and developed supercell characteristics once the second waterspout was in progress. Polarimetric characteristics of the storm, and of the development of supercell character, are presented. These observations represent the first documented polarimetric radar observations of waterspout-producing convection in the Great Lakes region. Unusually high differential reflectivity values accompanied this storm and its initiating boundary. The high values along the boundary are partially explained by a high density of dragonflies. High differential reflectivity values were present through much of the storm of interest despite very low aerosol concentration at low levels in the lake-influenced air mass. Finally, this case illustrates the importance of environmental awareness on waterspout-favorable days, especially when boundaries are nearby to serve as a potential source of enhanced environmental vertical vorticity. | ||
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10.1175/WAF-D-14-00114.1 doi PQ20160617 (DE-627)OLC1957752408 (DE-599)GBVOLC1957752408 (PRQ)c1856-a04d3abcf5ceebe1b0dcece65b438a4c0a8200efbcb5b57aa7afb10e1cf1e1b0 (KEY)0161211520150000030000200329polarimetricradarobservationsfromawaterspoutproduc DE-627 ger DE-627 rakwb eng 550 DNB 38.80 bkl Matthew S Van Den Broeke verfasserin aut Polarimetric Radar Observations from a Waterspout-Producing Thunderstorm 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier A family of four waterspouts was produced by a convective cell over western Lake Michigan on 12 September 2013. This storm initiated along a boundary north of a mesolow in a low-level cold-air advection regime, and developed supercell characteristics once the second waterspout was in progress. Polarimetric characteristics of the storm, and of the development of supercell character, are presented. These observations represent the first documented polarimetric radar observations of waterspout-producing convection in the Great Lakes region. Unusually high differential reflectivity values accompanied this storm and its initiating boundary. The high values along the boundary are partially explained by a high density of dragonflies. High differential reflectivity values were present through much of the storm of interest despite very low aerosol concentration at low levels in the lake-influenced air mass. Finally, this case illustrates the importance of environmental awareness on waterspout-favorable days, especially when boundaries are nearby to serve as a potential source of enhanced environmental vertical vorticity. Lakes Vortices Florida Keys Lake Michigan Tornadoes Great Lakes Meteorology Storms Bias Cynthia A Van Den Broeke oth Enthalten in Weather and forecasting Boston, Mass. : AMS, 1986 30(2015), 2, Seite 329-348 (DE-627)129242616 (DE-600)58730-8 (DE-576)330410768 0882-8156 nnns volume:30 year:2015 number:2 pages:329-348 http://dx.doi.org/10.1175/WAF-D-14-00114.1 Volltext http://search.proquest.com/docview/1674531190 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO GBV_ILN_601 38.80 AVZ AR 30 2015 2 329-348 |
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10.1175/WAF-D-14-00114.1 doi PQ20160617 (DE-627)OLC1957752408 (DE-599)GBVOLC1957752408 (PRQ)c1856-a04d3abcf5ceebe1b0dcece65b438a4c0a8200efbcb5b57aa7afb10e1cf1e1b0 (KEY)0161211520150000030000200329polarimetricradarobservationsfromawaterspoutproduc DE-627 ger DE-627 rakwb eng 550 DNB 38.80 bkl Matthew S Van Den Broeke verfasserin aut Polarimetric Radar Observations from a Waterspout-Producing Thunderstorm 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier A family of four waterspouts was produced by a convective cell over western Lake Michigan on 12 September 2013. This storm initiated along a boundary north of a mesolow in a low-level cold-air advection regime, and developed supercell characteristics once the second waterspout was in progress. Polarimetric characteristics of the storm, and of the development of supercell character, are presented. These observations represent the first documented polarimetric radar observations of waterspout-producing convection in the Great Lakes region. Unusually high differential reflectivity values accompanied this storm and its initiating boundary. The high values along the boundary are partially explained by a high density of dragonflies. High differential reflectivity values were present through much of the storm of interest despite very low aerosol concentration at low levels in the lake-influenced air mass. Finally, this case illustrates the importance of environmental awareness on waterspout-favorable days, especially when boundaries are nearby to serve as a potential source of enhanced environmental vertical vorticity. Lakes Vortices Florida Keys Lake Michigan Tornadoes Great Lakes Meteorology Storms Bias Cynthia A Van Den Broeke oth Enthalten in Weather and forecasting Boston, Mass. : AMS, 1986 30(2015), 2, Seite 329-348 (DE-627)129242616 (DE-600)58730-8 (DE-576)330410768 0882-8156 nnns volume:30 year:2015 number:2 pages:329-348 http://dx.doi.org/10.1175/WAF-D-14-00114.1 Volltext http://search.proquest.com/docview/1674531190 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO GBV_ILN_601 38.80 AVZ AR 30 2015 2 329-348 |
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10.1175/WAF-D-14-00114.1 doi PQ20160617 (DE-627)OLC1957752408 (DE-599)GBVOLC1957752408 (PRQ)c1856-a04d3abcf5ceebe1b0dcece65b438a4c0a8200efbcb5b57aa7afb10e1cf1e1b0 (KEY)0161211520150000030000200329polarimetricradarobservationsfromawaterspoutproduc DE-627 ger DE-627 rakwb eng 550 DNB 38.80 bkl Matthew S Van Den Broeke verfasserin aut Polarimetric Radar Observations from a Waterspout-Producing Thunderstorm 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier A family of four waterspouts was produced by a convective cell over western Lake Michigan on 12 September 2013. This storm initiated along a boundary north of a mesolow in a low-level cold-air advection regime, and developed supercell characteristics once the second waterspout was in progress. Polarimetric characteristics of the storm, and of the development of supercell character, are presented. These observations represent the first documented polarimetric radar observations of waterspout-producing convection in the Great Lakes region. Unusually high differential reflectivity values accompanied this storm and its initiating boundary. The high values along the boundary are partially explained by a high density of dragonflies. High differential reflectivity values were present through much of the storm of interest despite very low aerosol concentration at low levels in the lake-influenced air mass. Finally, this case illustrates the importance of environmental awareness on waterspout-favorable days, especially when boundaries are nearby to serve as a potential source of enhanced environmental vertical vorticity. Lakes Vortices Florida Keys Lake Michigan Tornadoes Great Lakes Meteorology Storms Bias Cynthia A Van Den Broeke oth Enthalten in Weather and forecasting Boston, Mass. : AMS, 1986 30(2015), 2, Seite 329-348 (DE-627)129242616 (DE-600)58730-8 (DE-576)330410768 0882-8156 nnns volume:30 year:2015 number:2 pages:329-348 http://dx.doi.org/10.1175/WAF-D-14-00114.1 Volltext http://search.proquest.com/docview/1674531190 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO GBV_ILN_601 38.80 AVZ AR 30 2015 2 329-348 |
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10.1175/WAF-D-14-00114.1 doi PQ20160617 (DE-627)OLC1957752408 (DE-599)GBVOLC1957752408 (PRQ)c1856-a04d3abcf5ceebe1b0dcece65b438a4c0a8200efbcb5b57aa7afb10e1cf1e1b0 (KEY)0161211520150000030000200329polarimetricradarobservationsfromawaterspoutproduc DE-627 ger DE-627 rakwb eng 550 DNB 38.80 bkl Matthew S Van Den Broeke verfasserin aut Polarimetric Radar Observations from a Waterspout-Producing Thunderstorm 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier A family of four waterspouts was produced by a convective cell over western Lake Michigan on 12 September 2013. This storm initiated along a boundary north of a mesolow in a low-level cold-air advection regime, and developed supercell characteristics once the second waterspout was in progress. Polarimetric characteristics of the storm, and of the development of supercell character, are presented. These observations represent the first documented polarimetric radar observations of waterspout-producing convection in the Great Lakes region. Unusually high differential reflectivity values accompanied this storm and its initiating boundary. The high values along the boundary are partially explained by a high density of dragonflies. High differential reflectivity values were present through much of the storm of interest despite very low aerosol concentration at low levels in the lake-influenced air mass. Finally, this case illustrates the importance of environmental awareness on waterspout-favorable days, especially when boundaries are nearby to serve as a potential source of enhanced environmental vertical vorticity. Lakes Vortices Florida Keys Lake Michigan Tornadoes Great Lakes Meteorology Storms Bias Cynthia A Van Den Broeke oth Enthalten in Weather and forecasting Boston, Mass. : AMS, 1986 30(2015), 2, Seite 329-348 (DE-627)129242616 (DE-600)58730-8 (DE-576)330410768 0882-8156 nnns volume:30 year:2015 number:2 pages:329-348 http://dx.doi.org/10.1175/WAF-D-14-00114.1 Volltext http://search.proquest.com/docview/1674531190 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO GBV_ILN_601 38.80 AVZ AR 30 2015 2 329-348 |
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10.1175/WAF-D-14-00114.1 doi PQ20160617 (DE-627)OLC1957752408 (DE-599)GBVOLC1957752408 (PRQ)c1856-a04d3abcf5ceebe1b0dcece65b438a4c0a8200efbcb5b57aa7afb10e1cf1e1b0 (KEY)0161211520150000030000200329polarimetricradarobservationsfromawaterspoutproduc DE-627 ger DE-627 rakwb eng 550 DNB 38.80 bkl Matthew S Van Den Broeke verfasserin aut Polarimetric Radar Observations from a Waterspout-Producing Thunderstorm 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier A family of four waterspouts was produced by a convective cell over western Lake Michigan on 12 September 2013. This storm initiated along a boundary north of a mesolow in a low-level cold-air advection regime, and developed supercell characteristics once the second waterspout was in progress. Polarimetric characteristics of the storm, and of the development of supercell character, are presented. These observations represent the first documented polarimetric radar observations of waterspout-producing convection in the Great Lakes region. Unusually high differential reflectivity values accompanied this storm and its initiating boundary. The high values along the boundary are partially explained by a high density of dragonflies. High differential reflectivity values were present through much of the storm of interest despite very low aerosol concentration at low levels in the lake-influenced air mass. Finally, this case illustrates the importance of environmental awareness on waterspout-favorable days, especially when boundaries are nearby to serve as a potential source of enhanced environmental vertical vorticity. Lakes Vortices Florida Keys Lake Michigan Tornadoes Great Lakes Meteorology Storms Bias Cynthia A Van Den Broeke oth Enthalten in Weather and forecasting Boston, Mass. : AMS, 1986 30(2015), 2, Seite 329-348 (DE-627)129242616 (DE-600)58730-8 (DE-576)330410768 0882-8156 nnns volume:30 year:2015 number:2 pages:329-348 http://dx.doi.org/10.1175/WAF-D-14-00114.1 Volltext http://search.proquest.com/docview/1674531190 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO GBV_ILN_601 38.80 AVZ AR 30 2015 2 329-348 |
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| title_sort |
polarimetric radar observations from a waterspout-producing thunderstorm |
| title_auth |
Polarimetric Radar Observations from a Waterspout-Producing Thunderstorm |
| abstract |
A family of four waterspouts was produced by a convective cell over western Lake Michigan on 12 September 2013. This storm initiated along a boundary north of a mesolow in a low-level cold-air advection regime, and developed supercell characteristics once the second waterspout was in progress. Polarimetric characteristics of the storm, and of the development of supercell character, are presented. These observations represent the first documented polarimetric radar observations of waterspout-producing convection in the Great Lakes region. Unusually high differential reflectivity values accompanied this storm and its initiating boundary. The high values along the boundary are partially explained by a high density of dragonflies. High differential reflectivity values were present through much of the storm of interest despite very low aerosol concentration at low levels in the lake-influenced air mass. Finally, this case illustrates the importance of environmental awareness on waterspout-favorable days, especially when boundaries are nearby to serve as a potential source of enhanced environmental vertical vorticity. |
| abstractGer |
A family of four waterspouts was produced by a convective cell over western Lake Michigan on 12 September 2013. This storm initiated along a boundary north of a mesolow in a low-level cold-air advection regime, and developed supercell characteristics once the second waterspout was in progress. Polarimetric characteristics of the storm, and of the development of supercell character, are presented. These observations represent the first documented polarimetric radar observations of waterspout-producing convection in the Great Lakes region. Unusually high differential reflectivity values accompanied this storm and its initiating boundary. The high values along the boundary are partially explained by a high density of dragonflies. High differential reflectivity values were present through much of the storm of interest despite very low aerosol concentration at low levels in the lake-influenced air mass. Finally, this case illustrates the importance of environmental awareness on waterspout-favorable days, especially when boundaries are nearby to serve as a potential source of enhanced environmental vertical vorticity. |
| abstract_unstemmed |
A family of four waterspouts was produced by a convective cell over western Lake Michigan on 12 September 2013. This storm initiated along a boundary north of a mesolow in a low-level cold-air advection regime, and developed supercell characteristics once the second waterspout was in progress. Polarimetric characteristics of the storm, and of the development of supercell character, are presented. These observations represent the first documented polarimetric radar observations of waterspout-producing convection in the Great Lakes region. Unusually high differential reflectivity values accompanied this storm and its initiating boundary. The high values along the boundary are partially explained by a high density of dragonflies. High differential reflectivity values were present through much of the storm of interest despite very low aerosol concentration at low levels in the lake-influenced air mass. Finally, this case illustrates the importance of environmental awareness on waterspout-favorable days, especially when boundaries are nearby to serve as a potential source of enhanced environmental vertical vorticity. |
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GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO GBV_ILN_601 |
| container_issue |
2 |
| title_short |
Polarimetric Radar Observations from a Waterspout-Producing Thunderstorm |
| url |
http://dx.doi.org/10.1175/WAF-D-14-00114.1 http://search.proquest.com/docview/1674531190 |
| remote_bool |
false |
| author2 |
Cynthia A Van Den Broeke |
| author2Str |
Cynthia A Van Den Broeke |
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129242616 |
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n |
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false |
| hochschulschrift_bool |
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| author2_role |
oth |
| doi_str |
10.1175/WAF-D-14-00114.1 |
| up_date |
2024-07-04T01:16:07.998Z |
| _version_ |
1803609196985319424 |
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