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dc.contributor.authorCooper, Owen R.
dc.contributor.authorSchultz, Martin G.
dc.contributor.authorSchroeder, Sabine
dc.contributor.authorChang, Kai-Lan
dc.contributor.authorGaudel, Audrey
dc.contributor.authorBenitez, Gerardo Carbajal
dc.contributor.authorCuevas, Emilio
dc.contributor.authorFrölich, Marina
dc.contributor.authorGalbally, Ian E.
dc.contributor.authorMolloy, Suzie
dc.contributor.authorKubistin, Dagmar
dc.contributor.authorLu, Xiao
dc.contributor.authorMcClure-Begley, Audra
dc.contributor.authorNédélec, Philippe
dc.contributor.authorO'Brien, Jason
dc.contributor.authorOltmans, Samuel J.
dc.contributor.authorPetropavlovskikh, Irina
dc.contributor.authorRies, Ludwig
dc.contributor.authorSenik, Irina
dc.contributor.authorSjöberg, Karin
dc.contributor.authorSolberg, Sverre
dc.contributor.authorSpain, Gerard T.
dc.contributor.authorSpangl, Wolfgang
dc.contributor.authorSteinbacher, Martin
dc.contributor.authorTarasick, David
dc.contributor.authorThouret, Valérie
dc.contributor.authorXu, Xiaobin
dc.date.accessioned2020-06-12T07:32:34Z
dc.date.available2020-06-12T07:32:34Z
dc.date.created2020-06-10T10:43:21Z
dc.date.issued2020
dc.identifier.citationElementa: Science of the Anthropocene. 2020, 8 .en_US
dc.identifier.issn2325-1026
dc.identifier.urihttps://hdl.handle.net/11250/2657815
dc.description.abstractExtracting globally representative trend information from lower tropospheric ozone observations is extremely difficult due to the highly variable distribution and interannual variability of ozone, and the ongoing shift of ozone precursor emissions from high latitudes to low latitudes. Here we report surface ozone trends at 27 globally distributed remote locations (20 in the Northern Hemisphere, 7 in the Southern Hemisphere), focusing on continuous time series that extend from the present back to at least 1995. While these sites are only representative of less than 25% of the global surface area, this analysis provides a range of regional long-term ozone trends for the evaluation of global chemistry-climate models. Trends are based on monthly mean ozone anomalies, and all sites have at least 20 years of data, which improves the likelihood that a robust trend value is due to changes in ozone precursor emissions and/or forced climate change rather than naturally occurring climate variability. Since 1995, the Northern Hemisphere sites are nearly evenly split between positive and negative ozone trends, while 5 of 7 Southern Hemisphere sites have positive trends. Positive trends are in the range of 0.5-2 ppbv decade-1, with ozone increasing at Mauna Loa by roughly 50% since the late 1950s. Two high elevation Alpine sites, discussed by previous assessments, exhibit decreasing ozone trends in contrast to the positive trend observed by IAGOS commercial aircraft in the European lower free-troposphere. The Alpine sites frequently sample polluted European boundary layer air, especially in summer, and can only be representative of lower free tropospheric ozone if the data are carefully filtered to avoid boundary layer air. The highly variable ozone trends at these 27 surface sites are not necessarily indicative of free tropospheric trends, which have been overwhelmingly positive since the mid-1990s, as shown by recent studies of ozonesonde and aircraft observations.en_US
dc.language.isoengen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleMulti-decadal surface ozone trends at globally distributed remote locationsen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.rights.holder© 2019 The Author(s)en_US
dc.source.pagenumber34en_US
dc.source.volume8en_US
dc.source.journalElementa: Science of the Anthropoceneen_US
dc.identifier.doi10.1525/elementa.420
dc.identifier.cristin1814734
dc.relation.projectNILU: 7726en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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