This HTML5 document contains 44 embedded RDF statements represented using HTML+Microdata notation.

The embedded RDF content will be recognized by any processor of HTML5 Microdata.

Namespace Prefixes

PrefixIRI
n19http://linked.opendata.cz/ontology/domain/vavai/riv/typAkce/
dctermshttp://purl.org/dc/terms/
n6http://purl.org/net/nknouf/ns/bibtex#
n7http://linked.opendata.cz/resource/domain/vavai/riv/tvurce/
n17http://linked.opendata.cz/ontology/domain/vavai/
n20https://schema.org/
n18http://linked.opendata.cz/resource/domain/vavai/zamer/
shttp://schema.org/
skoshttp://www.w3.org/2004/02/skos/core#
n3http://linked.opendata.cz/ontology/domain/vavai/riv/
n4http://linked.opendata.cz/resource/domain/vavai/vysledek/RIV%2F68378289%3A_____%2F04%3A00104027%21RIV%2F2005%2FAV0%2FA04005%2FN/
n2http://linked.opendata.cz/resource/domain/vavai/vysledek/
rdfhttp://www.w3.org/1999/02/22-rdf-syntax-ns#
n12http://linked.opendata.cz/ontology/domain/vavai/riv/klicoveSlovo/
n15http://linked.opendata.cz/ontology/domain/vavai/riv/duvernostUdaju/
xsdhhttp://www.w3.org/2001/XMLSchema#
n16http://linked.opendata.cz/ontology/domain/vavai/riv/aktivita/
n10http://linked.opendata.cz/ontology/domain/vavai/riv/jazykVysledku/
n14http://linked.opendata.cz/ontology/domain/vavai/riv/obor/
n9http://linked.opendata.cz/ontology/domain/vavai/riv/druhVysledku/
n11http://reference.data.gov.uk/id/gregorian-year/

Statements

Subject Item
n2:RIV%2F68378289%3A_____%2F04%3A00104027%21RIV%2F2005%2FAV0%2FA04005%2FN
rdf:type
n17:Vysledek skos:Concept
dcterms:description
Vertikální profily ozónu obvykle nepředstavují hladkou křivku s maximem na výškách blízko 20 km. V dolní stratosféře často vidíme tenké vrstvy silně zvýšeného nebo sníženého obsahu ozónu, zvané laminy. Počítáme charakteristiky lamin, počet lamin a obsah ozónu v laminách na profil, pro stanice středních a vysokých šířek severní polokoule s dlouhými řadami měření ozónových profilů. Vyhodnocujeme dlouhodobé chování charakteristik lamin a nalézáme od poloviny či počátku let 90-tých, kdežto předtím byla tendence záporná. Předkládáme model vysvětlující většinu variability přítomné ve studovaných časových řadách lamin a ukazujeme, že dlouhodobá variabilita ozónových lamin je převážně způsobena dynamickými faktory Ozone vertical profile is not usually represented by a smooth curve with maximum at a height of about 20 km. Frequently thin layers with strongly enhanced or lowered ozone content, called laminae, are observed in the lower stratosphere. We compute ozone laminae characteristics, number of laminae and ozone content in laminae per profile, for stations in the high and middle NH latitudes having long time series of ozone profile measurements. We evaluate the long-term pattern of these characteristics and find a positive tendency in the lamina characteristics since the early to mid 1990s, while a negative tendency occured during the 1970s and 1980s. We propose model explaining much of the variability present in the examined time series and show that the long-term variability of the ozone laminae is predominantly forced by dynamical factors Ozone vertical profile is not usually represented by a smooth curve with maximum at a height of about 20 km. Frequently thin layers with strongly enhanced or lowered ozone content, called laminae, are observed in the lower stratosphere. We compute ozone laminae characteristics, number of laminae and ozone content in laminae per profile, for stations in the high and middle NH latitudes having long time series of ozone profile measurements. We evaluate the long-term pattern of these characteristics and find a positive tendency in the lamina characteristics since the early to mid 1990s, while a negative tendency occured during the 1970s and 1980s. We propose model explaining much of the variability present in the examined time series and show that the long-term variability of the ozone laminae is predominantly forced by dynamical factors
dcterms:title
Ozone laminae and teleconnection patterns Ozone laminae and teleconnection patterns Laminy v ozónu a telekonexe
skos:prefLabel
Ozone laminae and teleconnection patterns Laminy v ozónu a telekonexe Ozone laminae and teleconnection patterns
skos:notation
RIV/68378289:_____/04:00104027!RIV/2005/AV0/A04005/N
n3:strany
421;422
n3:aktivita
n16:Z
n3:aktivity
Z(AV0Z3042911)
n3:dodaniDat
n11:2005
n3:domaciTvurceVysledku
n7:7020139 n7:9492933
n3:druhVysledku
n9:D
n3:duvernostUdaju
n15:S
n3:entitaPredkladatele
n4:predkladatel
n3:idSjednocenehoVysledku
578714
n3:idVysledku
RIV/68378289:_____/04:00104027
n3:jazykVysledku
n10:eng
n3:klicovaSlova
ozone profile; ozone laminae
n3:klicoveSlovo
n12:ozone%20laminae n12:ozone%20profile
n3:kontrolniKodProRIV
[CD80A2228228]
n3:mistoKonaniAkce
Kos
n3:mistoVydani
Athens
n3:nazevZdroje
Proceedings of the Quadrennial Ozone Symposium /20./
n3:obor
n14:DG
n3:pocetDomacichTvurcuVysledku
2
n3:pocetTvurcuVysledku
3
n3:rokUplatneniVysledku
n11:2004
n3:tvurceVysledku
Laštovička, Jan Križan, Peter Krzyšcin, J. W.
n3:typAkce
n19:WRD
n3:zahajeniAkce
2004-06-01+02:00
n3:zamer
n18:AV0Z3042911
s:numberOfPages
2
n6:hasPublisher
International Ozone Commission
n20:isbn
960-630-103-6