Radar precipitation echo motion in Hurricane Donna
Radar data consisting of about 3,800 precipitation echoes were obtained by analyzing film from several radars during the same time period in Hurricane Donna. These data are combined to illustrate for the first time the complete field of relatively simultaneous echo motion at almost all ranges and az...
| Autor: | |
|---|---|
| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 1965 |
| País: | México |
| Institución: | UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO |
| Repositorio: | Geofísica Internacional |
| Idioma: | español |
| OAI Identifier: | oai:revistagi.geofisica.unam.mx:article/1603 |
| Acceso en línea: | http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1603 |
| Access Level: | acceso abierto |
| Palabra clave: | Huracan Donna Azimut Eco de precipitación Radar Hurricane Donna Azimuth Precipitation echo |
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Radar precipitation echo motion in Hurricane DonnaMovimiento del eco de precipitación en radar del Huracán DonnaSenn, H. V.Huracan DonnaAzimutEco de precipitaciónRadarHurricane DonnaAzimuthPrecipitation echoRadarRadar data consisting of about 3,800 precipitation echoes were obtained by analyzing film from several radars during the same time period in Hurricane Donna. These data are combined to illustrate for the first time the complete field of relatively simultaneous echo motion at almost all ranges and azimuths in a hurricane. The field of radar echo motion in Hurricane Donna on 9 September 1960 is then compared with local surface and other winds; and also on 9 an d 10 September with radar precipitation echo motion data from Hurricanes Edna 1954, Connie, Diane and lone 1955, Audrey 1957, and Daisy and Helene 1958, When storm center velocity is eliminated, it is shown that the resulting relative echo motion maximums occur most often to the left of the direction. Possible explanations for this echo motion behavior are discussed.Analizando películas de varios radares del mismo tiempo en el Huracan Donna, se obtuvieron datos consistentes en casi 3,800 ecos de precipitación que se combinaron para ilustrar, por primera vez, el campo completo de movimientos de eco relativamente simultáneos en casi todas las alturas y azimutes de un huracán. EI campo de los movimientos de eco en radar del Huracan Donna, el 9 de septiembre de 1960, se comparó después con vientos locales de superficies y otro y también el 9 y 10 de septiembre con datos de movimientos de eco de precipitación en radar en los Huracanes Edna 1954, Connie, Diana e lone 1955, Audrey 1957 y Daisy y Helene 1958. Cuando se elimina Ia velocidad del centro de Ia tormenta, puede comprobarse que los máximos del movimiento de eco relativo resultante tienen Iugar con más frecuencia a Ia izquierda de esa dirección. Se discuten posibles explicaciones para este comportamiento del movimiento de eco.Universidad Nacional Autónoma de México. Instituto de Geofísica1965-07-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttp://revistagi.geofisica.unam.mx/index.php/RGI/article/view/160310.22201/igeof.00167169p.1965.5.3.1113Geofisica Internacional; Vol. 5 No. 3 (1965): July 1, 1965; 71-78Geofísica Internacional; Vol. 5 Núm. 3 (1965): Julio 1, 1965; 71-782954-436X0016-716910.22201/igeof.2954436xe.1965.5.3reponame:Geofísica Internacionalinstname:UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICOinstacron:UNAMspahttp://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1603/1715Derechos de autor 1965 Geofísica Internacionalhttps://creativecommons.org/licenses/by-nc-sa/4.0/info:eu-repo/semantics/openAccessoai:revistagi.geofisica.unam.mx:article/16032024-08-16T17:32:11Z |
| dc.title.none.fl_str_mv |
Radar precipitation echo motion in Hurricane Donna Movimiento del eco de precipitación en radar del Huracán Donna |
| title |
Radar precipitation echo motion in Hurricane Donna |
| spellingShingle |
Radar precipitation echo motion in Hurricane Donna Senn, H. V. Huracan Donna Azimut Eco de precipitación Radar Hurricane Donna Azimuth Precipitation echo Radar |
| title_short |
Radar precipitation echo motion in Hurricane Donna |
| title_full |
Radar precipitation echo motion in Hurricane Donna |
| title_fullStr |
Radar precipitation echo motion in Hurricane Donna |
| title_full_unstemmed |
Radar precipitation echo motion in Hurricane Donna |
| title_sort |
Radar precipitation echo motion in Hurricane Donna |
| dc.creator.none.fl_str_mv |
Senn, H. V. |
| author |
Senn, H. V. |
| author_facet |
Senn, H. V. |
| author_role |
author |
| dc.subject.none.fl_str_mv |
Huracan Donna Azimut Eco de precipitación Radar Hurricane Donna Azimuth Precipitation echo Radar |
| topic |
Huracan Donna Azimut Eco de precipitación Radar Hurricane Donna Azimuth Precipitation echo Radar |
| description |
Radar data consisting of about 3,800 precipitation echoes were obtained by analyzing film from several radars during the same time period in Hurricane Donna. These data are combined to illustrate for the first time the complete field of relatively simultaneous echo motion at almost all ranges and azimuths in a hurricane. The field of radar echo motion in Hurricane Donna on 9 September 1960 is then compared with local surface and other winds; and also on 9 an d 10 September with radar precipitation echo motion data from Hurricanes Edna 1954, Connie, Diane and lone 1955, Audrey 1957, and Daisy and Helene 1958, When storm center velocity is eliminated, it is shown that the resulting relative echo motion maximums occur most often to the left of the direction. Possible explanations for this echo motion behavior are discussed. |
| publishDate |
1965 |
| dc.date.none.fl_str_mv |
1965-07-01 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
| format |
article |
| status_str |
publishedVersion |
| dc.identifier.none.fl_str_mv |
http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1603 10.22201/igeof.00167169p.1965.5.3.1113 |
| url |
http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1603 |
| identifier_str_mv |
10.22201/igeof.00167169p.1965.5.3.1113 |
| dc.language.none.fl_str_mv |
spa |
| language |
spa |
| dc.relation.none.fl_str_mv |
http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1603/1715 |
| dc.rights.none.fl_str_mv |
Derechos de autor 1965 Geofísica Internacional https://creativecommons.org/licenses/by-nc-sa/4.0/ info:eu-repo/semantics/openAccess |
| rights_invalid_str_mv |
Derechos de autor 1965 Geofísica Internacional https://creativecommons.org/licenses/by-nc-sa/4.0/ |
| eu_rights_str_mv |
openAccess |
| dc.format.none.fl_str_mv |
application/pdf |
| dc.publisher.none.fl_str_mv |
Universidad Nacional Autónoma de México. Instituto de Geofísica |
| publisher.none.fl_str_mv |
Universidad Nacional Autónoma de México. Instituto de Geofísica |
| dc.source.none.fl_str_mv |
Geofisica Internacional; Vol. 5 No. 3 (1965): July 1, 1965; 71-78 Geofísica Internacional; Vol. 5 Núm. 3 (1965): Julio 1, 1965; 71-78 2954-436X 0016-7169 10.22201/igeof.2954436xe.1965.5.3 reponame:Geofísica Internacional instname:UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO instacron:UNAM |
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UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO |
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UNAM |
| institution |
UNAM |
| reponame_str |
Geofísica Internacional |
| collection |
Geofísica Internacional |
| repository.name.fl_str_mv |
|
| repository.mail.fl_str_mv |
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1858175399331102720 |
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15,811543 |