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Statements

Subject Item
n2:RIV%2F00020699%3A_____%2F11%3A%230000636%21RIV13-GA0-00020699
rdf:type
n10:Vysledek skos:Concept
dcterms:description
Recent observational and numerical modeling studies of the mechanisms which transport moisture to the stratosphere by deep convective storms at mid-latitudes are reviewed. Observational evidence of the cross-tropopause transport of moisture by thunderstorms includes satellite, aircraft and ground-based data. The primary satellite evidence is taken from both conventional satellite of thunderstorm images and CloudSat vertical cloud cross-section images. The conventional satellite images show cirrus plumes above the anvil tops of some of the convective storms where the anvils are already at the tropopause level. The CloudSat image shows an indication of penetration of cirrus plume into the stratosphere. The aircraft observations consist of earlier observations of the “jumping cirrus” phenomenon reported by Fujita and recent detection of ice particles in the stratospheric air associated with deep convective storms. The ground-based observations are video camera records of the jumping cirrus phenomenon occurring at the top of thunderstorm cells. Numerical model studies of the penetrative deep convective storms were performed utilizing a three-dimensional cloud dynamical model to simulate a typical severe storm which occurred in the US Midwest region on 2 August 1981. Model results indicate two physical mechanisms that cause water to be injected into the stratosphere from the storm: (1) the jumping cirrus mechanism which is caused by the gravity wave breaking at the cloud top, and (2) an instability caused by turbulent mixing in the outer shell of the overshooting dome. Implications of the penetrative convection on global processes and a brief future outlook are discussed. Recent observational and numerical modeling studies of the mechanisms which transport moisture to the stratosphere by deep convective storms at mid-latitudes are reviewed. Observational evidence of the cross-tropopause transport of moisture by thunderstorms includes satellite, aircraft and ground-based data. The primary satellite evidence is taken from both conventional satellite of thunderstorm images and CloudSat vertical cloud cross-section images. The conventional satellite images show cirrus plumes above the anvil tops of some of the convective storms where the anvils are already at the tropopause level. The CloudSat image shows an indication of penetration of cirrus plume into the stratosphere. The aircraft observations consist of earlier observations of the “jumping cirrus” phenomenon reported by Fujita and recent detection of ice particles in the stratospheric air associated with deep convective storms. The ground-based observations are video camera records of the jumping cirrus phenomenon occurring at the top of thunderstorm cells. Numerical model studies of the penetrative deep convective storms were performed utilizing a three-dimensional cloud dynamical model to simulate a typical severe storm which occurred in the US Midwest region on 2 August 1981. Model results indicate two physical mechanisms that cause water to be injected into the stratosphere from the storm: (1) the jumping cirrus mechanism which is caused by the gravity wave breaking at the cloud top, and (2) an instability caused by turbulent mixing in the outer shell of the overshooting dome. Implications of the penetrative convection on global processes and a brief future outlook are discussed.
dcterms:title
Cross Tropopause Transport of Water by Mid-Latitude Deep Convective Storms: A Review Cross Tropopause Transport of Water by Mid-Latitude Deep Convective Storms: A Review
skos:prefLabel
Cross Tropopause Transport of Water by Mid-Latitude Deep Convective Storms: A Review Cross Tropopause Transport of Water by Mid-Latitude Deep Convective Storms: A Review
skos:notation
RIV/00020699:_____/11:#0000636!RIV13-GA0-00020699
n10:predkladatel
n11:ico%3A00020699
n3:aktivita
n17:P
n3:aktivity
P(GA205/07/0905)
n3:cisloPeriodika
5
n3:dodaniDat
n9:2013
n3:domaciTvurceVysledku
n5:6117236 n5:3134083
n3:druhVysledku
n16:J
n3:duvernostUdaju
n15:S
n3:entitaPredkladatele
n14:predkladatel
n3:idSjednocenehoVysledku
192300
n3:idVysledku
RIV/00020699:_____/11:#0000636
n3:jazykVysledku
n4:eng
n3:klicovaSlova
thunderstorms; stratospheric water; convective transport; gravity wave breaking; above anvil plumes
n3:klicoveSlovo
n12:gravity%20wave%20breaking n12:stratospheric%20water n12:thunderstorms n12:convective%20transport n12:above%20anvil%20plumes
n3:kodStatuVydavatele
TW - Čínská republika (Tchaj-wan)
n3:kontrolniKodProRIV
[774C9DA75992]
n3:nazevZdroje
Terrestrial, Atmospheric and Oceanic Sciences
n3:obor
n13:DG
n3:pocetDomacichTvurcuVysledku
2
n3:pocetTvurcuVysledku
5
n3:projekt
n18:GA205%2F07%2F0905
n3:rokUplatneniVysledku
n9:2011
n3:svazekPeriodika
22
n3:tvurceVysledku
Šťástka, Jindřich Su, Shih-Hao Lin, H-M. Wang, P. K. Charvát, Zdeněk
s:issn
1017-0839
s:numberOfPages
16