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Statements

Subject Item
n2:RIV%2F68378289%3A_____%2F06%3A00044752%21RIV07-AV0-68378289
rdf:type
n7:Vysledek skos:Concept
dcterms:description
Měřené profily ozónu často vykazují úzké vrstvy zvýšené (kladné laminy) nebo snížené (záporné laminy) koncentrace ozónu. Nalezli jsme velké rozdíly mezi charakteristikami ozónových lamin na severní a jižní polokouli. Celkový nárůst (deficit) ozónu v kladných (záporných) laminách v profilu je daleko menší na jižní oproti severní polokouli. Na jižní polokouli jsme nepozorovali prokazatelný trend v charakteristikách lamin, kdežto na severní polokouli jsme pozorovali silný záporný trend s obratem ke kladnému trendu okolo r. 1995. Některé dynamické faktory, hlavně stupeň stability polárního víru, přispívají k dlouhodobému chování ozónových lamin. The measured ozone profiles often exhibit narrow layers of enhanced ozone concentration (positive laminae) or depleted ozone (negative laminae). We found large differences between the ozone laminae characteristics in the Northern and Southern Hemisphere. The overall ozone content (deficit) in the positive (negative) laminae per profile and the number of laminae is much smaller in the Southern Hemisphere compared with the Northern Hemisphere. No detectable trend in lamina characteristics was observed in the Southern Hemisphere contrary to a strong negative trend with a reversal to strong positive trend in the mid-1990s in the Northern Hemisphere. Some dynamical factors, mainly the degree of stability of the polar vortex, are suggested as contributing to the long-term behavior of lamina characteristics. The measured ozone profiles often exhibit narrow layers of enhanced ozone concentration (positive laminae) or depleted ozone (negative laminae). We found large differences between the ozone laminae characteristics in the Northern and Southern Hemisphere. The overall ozone content (deficit) in the positive (negative) laminae per profile and the number of laminae is much smaller in the Southern Hemisphere compared with the Northern Hemisphere. No detectable trend in lamina characteristics was observed in the Southern Hemisphere contrary to a strong negative trend with a reversal to strong positive trend in the mid-1990s in the Northern Hemisphere. Some dynamical factors, mainly the degree of stability of the polar vortex, are suggested as contributing to the long-term behavior of lamina characteristics.
dcterms:title
Ozónové laminy: Srovnání jižní a severní polokoule a možné vysvětlení trendů Ozone laminae: Comparison of the Southern and Northern Hemisphere, and tentative explanation of trends Ozone laminae: Comparison of the Southern and Northern Hemisphere, and tentative explanation of trends
skos:prefLabel
Ozónové laminy: Srovnání jižní a severní polokoule a možné vysvětlení trendů Ozone laminae: Comparison of the Southern and Northern Hemisphere, and tentative explanation of trends Ozone laminae: Comparison of the Southern and Northern Hemisphere, and tentative explanation of trends
skos:notation
RIV/68378289:_____/06:00044752!RIV07-AV0-68378289
n3:strany
1962;1972
n3:aktivita
n10:Z
n3:aktivity
Z(AV0Z30420517)
n3:cisloPeriodika
17
n3:dodaniDat
n12:2007
n3:domaciTvurceVysledku
n11:9492933 n11:7020139
n3:druhVysledku
n4:J
n3:duvernostUdaju
n8:S
n3:entitaPredkladatele
n17:predkladatel
n3:idSjednocenehoVysledku
491343
n3:idVysledku
RIV/68378289:_____/06:00044752
n3:jazykVysledku
n14:eng
n3:klicovaSlova
Atmospheric ozone; Ozone laminae; Long-term trends
n3:klicoveSlovo
n6:Ozone%20laminae n6:Long-term%20trends n6:Atmospheric%20ozone
n3:kodStatuVydavatele
GB - Spojené království Velké Británie a Severního Irska
n3:kontrolniKodProRIV
[EAFCB26D4E05]
n3:nazevZdroje
Journal of Atmospheric and Solar-Terrestrial Physics
n3:obor
n15:DG
n3:pocetDomacichTvurcuVysledku
2
n3:pocetTvurcuVysledku
2
n3:rokUplatneniVysledku
n12:2006
n3:svazekPeriodika
68
n3:tvurceVysledku
Križan, Peter Laštovička, Jan
n3:zamer
n16:AV0Z30420517
s:issn
1364-6826
s:numberOfPages
11