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Statements

Subject Item
n2:RIV%2F68378289%3A_____%2F11%3A00367983%21RIV12-AV0-68378289
rdf:type
skos:Concept n11:Vysledek
rdfs:seeAlso
http://www.sciencedirect.com/science/article/pii/S0273117711005436
dcterms:description
This paper deals with the behavior of the annual cycle of total ozone (ACO3) and its amplitude (O3AMP) in the latitudinal belt from 20° N to 60° N. The prominent feature of the O3AMP spatial pattern is the sharp maximum over the north-east coast of Asia. Regarding temporal evolution of O3AMP we detected distinct negative trend in the period of 1979-1995 which is caused by stronger negative trend of maxima than the negative trend of minima in ACO3. In the period 1995-2008 we found the positive trend of ACO3 in most regions due to stronger positive trend of maxima than that of minima in ACO3 in the middle latitudes (especially over the central and northern Europe and the north-east Asia). In the lower latitudes a weak negative trend of O3AMP was identified and linked to weaker positive trend of maxima than positive trend of minima in ACO3. The behavior of the temporal trends was linked to the changes in Brewer-Dobson circulation and to the trends of tropopause pressure. This paper deals with the behavior of the annual cycle of total ozone (ACO3) and its amplitude (O3AMP) in the latitudinal belt from 20° N to 60° N. The prominent feature of the O3AMP spatial pattern is the sharp maximum over the north-east coast of Asia. Regarding temporal evolution of O3AMP we detected distinct negative trend in the period of 1979-1995 which is caused by stronger negative trend of maxima than the negative trend of minima in ACO3. In the period 1995-2008 we found the positive trend of ACO3 in most regions due to stronger positive trend of maxima than that of minima in ACO3 in the middle latitudes (especially over the central and northern Europe and the north-east Asia). In the lower latitudes a weak negative trend of O3AMP was identified and linked to weaker positive trend of maxima than positive trend of minima in ACO3. The behavior of the temporal trends was linked to the changes in Brewer-Dobson circulation and to the trends of tropopause pressure.
dcterms:title
Long term variability of total ozone yearly minima and maxima in the latitudinal belt from 20° N to 60° N derived from the merged satellite data in the period 1979-2008 Long term variability of total ozone yearly minima and maxima in the latitudinal belt from 20° N to 60° N derived from the merged satellite data in the period 1979-2008
skos:prefLabel
Long term variability of total ozone yearly minima and maxima in the latitudinal belt from 20° N to 60° N derived from the merged satellite data in the period 1979-2008 Long term variability of total ozone yearly minima and maxima in the latitudinal belt from 20° N to 60° N derived from the merged satellite data in the period 1979-2008
skos:notation
RIV/68378289:_____/11:00367983!RIV12-AV0-68378289
n11:predkladatel
n20:ico%3A68378289
n3:aktivita
n14:Z n14:P
n3:aktivity
P(GAP209/10/1792), P(ME10077), Z(AV0Z30420517), Z(MSM0021620860)
n3:cisloPeriodika
-
n3:dodaniDat
n10:2012
n3:domaciTvurceVysledku
n5:9492933
n3:druhVysledku
n9:J
n3:duvernostUdaju
n13:S
n3:entitaPredkladatele
n19:predkladatel
n3:idSjednocenehoVysledku
209905
n3:idVysledku
RIV/68378289:_____/11:00367983
n3:jazykVysledku
n18:eng
n3:klicovaSlova
annual cycle; total ozone; trends in annual cycle; long–term trends
n3:klicoveSlovo
n4:annual%20cycle n4:trends%20in%20annual%20cycle n4:long%E2%80%93term%20trends n4:total%20ozone
n3:kodStatuVydavatele
GB - Spojené království Velké Británie a Severního Irska
n3:kontrolniKodProRIV
[D2709B40C56C]
n3:nazevZdroje
Advances in Space Research
n3:obor
n12:DG
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
5
n3:projekt
n8:GAP209%2F10%2F1792 n8:ME10077
n3:rokUplatneniVysledku
n10:2011
n3:svazekPeriodika
48
n3:tvurceVysledku
Bai, J. H. Kozubek, M. Mikšovský, J. Wang, G. C. Križan, Peter
n3:wos
000296998300009
n3:zamer
n17:AV0Z30420517 n17:MSM0021620860
s:issn
0273-1177
s:numberOfPages
7
n15:doi
10.1016/j.asr.2011.07.010