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MOISTURE DETECTION ABOVE CONVECTIVE STORMS UTILIZING THE METHOD OF BRIGHTNESS TEMPERATURE DIFFERENCES BETWEEN WATER VAPOR AND IR WINDOW BANDS, BASED ON 2008 MSG RAPID SCAN SERVICE DATA

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F10%3A10106863" target="_blank" >RIV/00216208:11320/10:10106863 - isvavai.cz</a>

  • Alternative codes found

    RIV/00020699:_____/10:#0000624

  • Result on the web

    <a href="http://www.eumetsat.int/Home/Main/AboutEUMETSAT/Publications/ConferenceandWorkshopProceedings/2010/groups/cps/documents/document/pdf_conf_p57_s7_11_stastka_v.pdf" target="_blank" >http://www.eumetsat.int/Home/Main/AboutEUMETSAT/Publications/ConferenceandWorkshopProceedings/2010/groups/cps/documents/document/pdf_conf_p57_s7_11_stastka_v.pdf</a>

  • DOI - Digital Object Identifier

Alternative languages

  • Result language

    angličtina

  • Original language name

    MOISTURE DETECTION ABOVE CONVECTIVE STORMS UTILIZING THE METHOD OF BRIGHTNESS TEMPERATURE DIFFERENCES BETWEEN WATER VAPOR AND IR WINDOW BANDS, BASED ON 2008 MSG RAPID SCAN SERVICE DATA

  • Original language description

    The BTD method based on the Brightness Temperature Difference between WV and IR window bands has been used in previous studies to document the presence of water vapor above the tops of convective storms. This lower stratospheric moisture (LSM) can eitherbe advected above the storms from remote locations, or injected into the lower stratosphere by the storm itself. Previous studies either addressed cases observed by polar orbiting satellites (thus being only "snapshots"), or presented individual cases documented by MSG/SEVIRI 15-min. data. The present study focuses on this topic using a large dataset of cases collected during the 2008 season, documenting the hypothesized above-storm-LSM by means of MSG Rapid Scan Service 5-min. data. Besides the detection and statistics of LSM based on this dataset, we will also try to determine if any particular storm type tends to generate enhanced LSM, including the life cycle of these storms, and at what time the storm becomes the most efficient at

  • Czech name

  • Czech description

Classification

  • Type

    D - Article in proceedings

  • CEP classification

    DG - Atmospheric sciences, meteorology

  • OECD FORD branch

Result continuities

  • Project

    <a href="/en/project/GA205%2F07%2F0905" target="_blank" >GA205/07/0905: Exploitation of remote sensing means for modelling and monitoring of convective storms</a><br>

  • Continuities

    S - Specificky vyzkum na vysokych skolach

Others

  • Publication year

    2010

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Article name in the collection

    2010 EUMETSAT Meteorological Satellite Conference. Proceedings

  • ISBN

    978-92-9110-089-7

  • ISSN

    1011-3932

  • e-ISSN

  • Number of pages

    8

  • Pages from-to

    1-8

  • Publisher name

    EUMETSAT

  • Place of publication

    Darmstadt

  • Event location

    Córdoba

  • Event date

    Sep 20, 2010

  • Type of event by nationality

    EUR - Evropská akce

  • UT code for WoS article