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  • This paper addresses some of the early results of a study of various storm-top features by means of A-Train observations. While most of these features have already been documented in the 1980''s and 1990''s, there are still some uncertainties in their interpretation. These features include: 1) specific features in the IR brightness temperature field (coldest spots related to overshooting tops, warm spots forming downwind of them, cold-U shapes or cold rings), 2) overshooting tops, 3) increased cloud-top reflectivity in the 3.7/3.9 μm bands (related to cloud-top microphysics), 4) above-anvil plumes and jumping cirrus, 5) gravity waves, and 6) lower stratospheric water vapor provided by storm activity. The goal of this study is to achieve a better understanding of these phenomena, using the unique instrumentation of some of the A-Train satellites. Results of this study will contribute to a better interpretation and utilization of satellite data when monitoring and nowcasting deep convective storms.
  • This paper addresses some of the early results of a study of various storm-top features by means of A-Train observations. While most of these features have already been documented in the 1980''s and 1990''s, there are still some uncertainties in their interpretation. These features include: 1) specific features in the IR brightness temperature field (coldest spots related to overshooting tops, warm spots forming downwind of them, cold-U shapes or cold rings), 2) overshooting tops, 3) increased cloud-top reflectivity in the 3.7/3.9 μm bands (related to cloud-top microphysics), 4) above-anvil plumes and jumping cirrus, 5) gravity waves, and 6) lower stratospheric water vapor provided by storm activity. The goal of this study is to achieve a better understanding of these phenomena, using the unique instrumentation of some of the A-Train satellites. Results of this study will contribute to a better interpretation and utilization of satellite data when monitoring and nowcasting deep convective storms. (en)
Title
  • STUDY OF CONVECTIVE STORM-TOP FEATURES USING DATA FROM THE A-TRAIN SATELLITES
  • STUDY OF CONVECTIVE STORM-TOP FEATURES USING DATA FROM THE A-TRAIN SATELLITES (en)
skos:prefLabel
  • STUDY OF CONVECTIVE STORM-TOP FEATURES USING DATA FROM THE A-TRAIN SATELLITES
  • STUDY OF CONVECTIVE STORM-TOP FEATURES USING DATA FROM THE A-TRAIN SATELLITES (en)
skos:notation
  • RIV/00020699:_____/10:#0000628!RIV13-GA0-00020699
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GA205/07/0905), S
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 290751
http://linked.open...ai/riv/idVysledku
  • RIV/00020699:_____/10:#0000628
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • convective storm; cold-ring shape; cold-U shape; above-anvil plume; brightness temperature difference (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...ontrolniKodProRIV
  • [9D5CFFCAF77A]
http://linked.open...v/mistoKonaniAkce
  • Córdoba
http://linked.open...i/riv/mistoVydani
  • Darmstadt
http://linked.open...i/riv/nazevZdroje
  • 2010 EUMETSAT Meteorological Satellite Conference. Proceedings
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...iv/tvurceVysledku
  • Charvát, Zdeněk
  • Šťástka, Jindřich
  • Bedka, K.
  • Setvák, Martin
  • Lindsey, D. T.
  • Sokol, A.
http://linked.open...vavai/riv/typAkce
http://linked.open.../riv/zahajeniAkce
issn
  • 1011-3932
number of pages
http://purl.org/ne...btex#hasPublisher
  • EUMETSAT
https://schema.org/isbn
  • 978-92-9110-089-7
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