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The key role of diabatic processes in modifying the upper‐tropospheric wave guide: a North Atlantic case‐study

2011· article· en· 356 citations· W1986478868 on OpenAlex· 10.1002/qj.891

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Opus teacher head0.030
GPT teacher head0.232
Teacher spread
0.202 · how far apart the two teachers sit on this one work
Validation status
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Abstract

Abstract This study highlights the importance of diabatic processes for the complex interaction of weather systems in the North Atlantic–European sector during the week of 7–14 September 2008. A chain of events occurred including the extratropical transition (ET) of hurricane Hanna , a subsequently developing extratropical cyclone, the formation of an upper‐level potential vorticity (PV) streamer that protruded towards Europe and triggered intense rainfall, and the genesis of a Mediterranean cyclone. A PV perspective is adopted along with trajectory calculations to elucidate the diabatic modification of the midlatitude flow. Important diabatic PV modifications occurred at upper levels, associated with the cross‐isentropic transport of low‐PV air within warm conveyor belts (WCBs). These were diagnosed during the ET of Hanna and the development of the extratropical cyclone near Newfoundland. The WCBs contributed to the amplification of ridges downstream of each cyclone and to the subsequent elongation of Hanna 's upstream trough into a PV streamer. This streamer eventually triggered the Mediterranean cyclogenesis. The second major effect of the diabatic processes occurred on smaller scales, in the low and middle troposphere. The remnants of Hanna 's tropical PV core advected moist air towards the baroclinic zone leading to condensational PV production in the lower troposphere. In contrast, in the case of the extratropical cyclone, diabatic PV production occurred within its WCB at mid levels. These diagnostic analyses corroborate the potential of diabatic processes associated with extratropical flow systems for the modification of both the low‐level vortices and the upper‐level Rossby wave guide. Copyright © 2011 Royal Meteorological Society

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The record

Venue
Quarterly Journal of the Royal Meteorological Society
Topic
Tropical and Extratropical Cyclones Research
Field
Earth and Planetary Sciences
Canadian institutions
Funders
Keywords
Extratropical cycloneDiabaticClimatologyCyclogenesisPotential vorticityCyclone (programming language)TroposphereBaroclinityWesterliesMiddle latitudesAtmospheric sciencesEnvironmental scienceGeologyRossby waveMeteorologyVorticityVortexGeographyPhysicsAdiabatic process
Has abstract in OpenAlex
yes