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Statements

Subject Item
n2:RIV%2F00216208%3A11320%2F12%3A10132765%21RIV13-GA0-11320___
rdf:type
n11:Vysledek skos:Concept
rdfs:seeAlso
http://dx.doi.org/10.1007/s10584-011-0147-0
dcterms:description
Oscillations in the period band of 10-12 years were globally analyzed by the pseudo-2D wavelet transform of reanalyzed (ERA-40 and NCEP/NCAR) and HadAT radiosonde series at several pressure levels. The results were obtained for the series of temperature, u and v wind velocities, ozone mass mixing ratios at pressure levels up to 10 hPa and temperature and height of the tropopause. The study provides a detailed description of the oscillations' spatial distribution, together with mutual comparison of the reanalyzed datasets. The analysis is supplemented by a correlation study between the wavelet power spectra interval of the reanalyzed and radiosonde series. For the temperature series, the study shows that the cycle is detected primarily in the tropics and subtropics; the details of the spatial patterns, however, differ significantly for the ERA-40 and NCEP/NCAR series. The analysis of the u and v velocities provides a new characterization of the longitudinal variability of the regions sensitive to solar forcing showing, e.g., preferences for Pacific Ocean areas at 100 hPa. In the ozone mass mixing ratio fields, the oscillations are identified throughout hemispherically asymmetrical and vertically variable locations. The findings describe cycle spatial distribution in a new way and are in general agreement with other studies. The analysis of the temperature and height of the tropopause showed that the regions where the cycle is detected are primarily found within tropical to middle latitudes, with pronounced longitudinal variability over the eastern Pacific Ocean. Oscillations in the period band of 10-12 years were globally analyzed by the pseudo-2D wavelet transform of reanalyzed (ERA-40 and NCEP/NCAR) and HadAT radiosonde series at several pressure levels. The results were obtained for the series of temperature, u and v wind velocities, ozone mass mixing ratios at pressure levels up to 10 hPa and temperature and height of the tropopause. The study provides a detailed description of the oscillations' spatial distribution, together with mutual comparison of the reanalyzed datasets. The analysis is supplemented by a correlation study between the wavelet power spectra interval of the reanalyzed and radiosonde series. For the temperature series, the study shows that the cycle is detected primarily in the tropics and subtropics; the details of the spatial patterns, however, differ significantly for the ERA-40 and NCEP/NCAR series. The analysis of the u and v velocities provides a new characterization of the longitudinal variability of the regions sensitive to solar forcing showing, e.g., preferences for Pacific Ocean areas at 100 hPa. In the ozone mass mixing ratio fields, the oscillations are identified throughout hemispherically asymmetrical and vertically variable locations. The findings describe cycle spatial distribution in a new way and are in general agreement with other studies. The analysis of the temperature and height of the tropopause showed that the regions where the cycle is detected are primarily found within tropical to middle latitudes, with pronounced longitudinal variability over the eastern Pacific Ocean.
dcterms:title
Imprint of the 11-year solar cycle in reanalyzed and radiosonde datasets: a spatial frequency analysis approach Imprint of the 11-year solar cycle in reanalyzed and radiosonde datasets: a spatial frequency analysis approach
skos:prefLabel
Imprint of the 11-year solar cycle in reanalyzed and radiosonde datasets: a spatial frequency analysis approach Imprint of the 11-year solar cycle in reanalyzed and radiosonde datasets: a spatial frequency analysis approach
skos:notation
RIV/00216208:11320/12:10132765!RIV13-GA0-11320___
n11:predkladatel
n12:orjk%3A11320
n3:aktivita
n19:I n19:P
n3:aktivity
I, P(GP205/07/P199)
n3:cisloPeriodika
1-2
n3:dodaniDat
n13:2013
n3:domaciTvurceVysledku
n7:8002002 n7:6594425 n7:6598986 n7:9830707 n7:4582411
n3:druhVysledku
n20:J
n3:duvernostUdaju
n14:S
n3:entitaPredkladatele
n8:predkladatel
n3:idSjednocenehoVysledku
140903
n3:idVysledku
RIV/00216208:11320/12:10132765
n3:jazykVysledku
n5:eng
n3:klicovaSlova
qbo; centuries; ozone; signal; wavelet analysis; stratospheric temperature; sunspot cycle; quasi-biennial oscillation
n3:klicoveSlovo
n4:ozone n4:qbo n4:stratospheric%20temperature n4:signal n4:wavelet%20analysis n4:quasi-biennial%20oscillation n4:sunspot%20cycle n4:centuries
n3:kodStatuVydavatele
NL - Nizozemsko
n3:kontrolniKodProRIV
[67A3B7AC1D50]
n3:nazevZdroje
Climatic Change
n3:obor
n15:DG
n3:pocetDomacichTvurcuVysledku
5
n3:pocetTvurcuVysledku
5
n3:projekt
n18:GP205%2F07%2FP199
n3:rokUplatneniVysledku
n13:2012
n3:svazekPeriodika
110
n3:tvurceVysledku
Mikšovský, Jiří Žák, Michal Huszár, Peter Pišoft, Petr Holtanová, Eva
n3:wos
000297910300006
s:issn
0165-0009
s:numberOfPages
15
n10:doi
10.1007/s10584-011-0147-0
n17:organizacniJednotka
11320