Diferencia entre revisiones de «Frente de ráfaga»

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Gust fronts create low-level [[wind shear]] which can be hazardous to planes when they takeoff or land.<ref>{{cite journal|author=Diana L. Klingle, David R. Smith, and Marilyn M. Wolfson|url=http://ams.allenpress.com/perlserv/?request=get-abstract&doi=10.1175%2F1520-0493(1987)115%3C0905%3AGFCADB%3E2.0.CO%3B2|title=Gust Front Characteristics as Detected by Doppler Radar|accessdate=2008-07-09|journal=Monthly Weather Review|pages=905-918|volume=115|number=5|date=May 1987}}</ref> Flying [[insect]]s, a subset of [[arthropods]], are swept along by the [[prevailing winds]].<ref>{{cite web|author=Diana Yates|date=2008|url=http://news.illinois.edu/news/08/0707birds.html|title=Birds migrate together at night in dispersed flocks, new study indicates|publisher=[[University of Illinois]] at Urbana - Champaign|accessdate=2009-04-26}}</ref> As such, fine line patterns within [[weather radar]] imagery, associated with converging winds, are dominated by insect returns.<ref>{{cite web|author=Bart Geerts and Dave Leon|date=2003|url=http://www-das.uwyo.edu/wcr/projects/ihop02/coldfront_preprint.pdf|title=P5A.6 Fine-Scale Vertical Structure of a Cold Front As Revealed By Airborne 95 GHZ Radar|publisher=[[University of Wyoming]]|accessdate=2009-04-26}}</ref> At the surface, clouds of dust can be raised by outflow boundaries. If squall lines form over arid regions, a duststorm known as a [[haboob]] may result from the high winds in their wake picking up dust from the desert floor.<ref>{{cite web|author=Western Region Climate Center|date=2002|url=http://www.wrcc.dri.edu/ams/glossary.html#H|title=H|publisher=Desert Research Institute|accessdate=2006-10-22}}</ref> If outflow boundaries move into areas of the atmosphere which are stable in the low levels, such as over colder pockets of ocean or through the cold sector of [[extratropical cyclone]]s, they can create a phenomenon known as an undular bore, which shows up on satellite and radar imagery as a series of [[transverse wave]]s in the cloud field oriented perpendicular to the low-level winds.<ref>{{cite web|url=http://www.arpal.org/Pubbl/paper/eumetsat-mauritania.pdf|title=Outflow from convective storm, Mauritania and adjacent Atlantic Ocean (13 August 2006)|author=Martin Setvak, Jochen Kerkmann, Alexander Jacob, HansPeter Roesli, Stefano Gallino, and Daniel Lindsey|accessdate=2009-07-03|date=2007-03-19|publisher=Agenzia Regionale per la Protezione dell'Ambiente Ligure}}</ref>
== EnlacesVéase internostambién ==
* [[Densidad]]
* [[Gustnado]]
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