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
Identifikátory výsledku
Kód výsledku v 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>
Nalezeny alternativní kódy
RIV/00020699:_____/10:#0000624
Výsledek na webu
<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
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Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
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
Popis výsledku v původním jazyce
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
Název v anglickém jazyce
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
Popis výsledku anglicky
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
Klasifikace
Druh
D - Stať ve sborníku
CEP obor
DG - Vědy o atmosféře, meteorologie
OECD FORD obor
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Návaznosti výsledku
Projekt
<a href="/cs/project/GA205%2F07%2F0905" target="_blank" >GA205/07/0905: Využití distančních měření při modelování a monitorování silných konvektivních bouří</a><br>
Návaznosti
S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2010
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název statě ve sborníku
2010 EUMETSAT Meteorological Satellite Conference. Proceedings
ISBN
978-92-9110-089-7
ISSN
1011-3932
e-ISSN
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Počet stran výsledku
8
Strana od-do
1-8
Název nakladatele
EUMETSAT
Místo vydání
Darmstadt
Místo konání akce
Córdoba
Datum konání akce
20. 9. 2010
Typ akce podle státní příslušnosti
EUR - Evropská akce
Kód UT WoS článku
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