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LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00006503naa a2200829 4500
001oai:gup.ub.gu.se/269046
003SwePub
008240528s2018 | |||||||||||000 ||eng|
009oai:research.chalmers.se:e46ad2c2-8e50-4060-8e42-5bb32980a8a7
024a https://gup.ub.gu.se/publication/2690462 URI
024a https://doi.org/10.1525/elementa.3022 DOI
024a https://research.chalmers.se/publication/5059022 URI
040 a (SwePub)gud (SwePub)cth
041 a eng
042 9 SwePub
072 7a ref2 swepub-contenttype
072 7a art2 swepub-publicationtype
100a Mills, Gina,d 1959u Gothenburg University,Göteborgs universitet,Institutionen för biologi och miljövetenskap,Department of Biological and Environmental Sciences,UK Centre For Ecology & Hydrology (UKCEH),University of Gothenburg4 aut0 (Swepub:gu)xmilgi
2451 0a Tropospheric Ozone Assessment Report: Present-day tropospheric ozone distribution and trends relevant to vegetation
264 c 2018-06-28
264 1b University of California Press,c 2018
520 a This Tropospheric Ozone Assessment Report (TOAR) on the current state of knowledge of ozone metrics of relevance to vegetation (TOAR-Vegetation) reports on present-day global distribution of ozone at over 3300 vegetated sites and the long-term trends at nearly 1200 sites. TOAR-Vegetation focusses on three metrics over vegetation-relevant time-periods across major world climatic zones: M12, the mean ozone during 08:00-19:59; AOT40, the accumulation of hourly mean ozone values over 40 ppb during daylight hours, and W126 with stronger weighting to higher hourly mean values, accumulated during 08:00-19:59. Although the density of measurement stations is highly variable across regions, in general, the highest ozone values (mean, 2010-14) are in mid-latitudes of the northern hemisphere, including southern USA, the Mediterranean basin, northern India, north, north-west and east China, the Republic of Korea and Japan. The lowest metric values reported are in Australia, New Zealand, southern parts of South America and some northern parts of Europe, Canada and the USA. Regional-scale assessments showed, for example, significantly higher AOT40 and W126 values in East Asia (EAS) than Europe (EUR) in wheat growing areas (p < 0.05), but not in rice growing areas. In NAM, the dominant trend during 1995-2014 was a significant decrease in ozone, whilst in EUR it was no change and in EAS it was a significant increase. TOAR-Vegetation provides recommendations to facilitate a more complete global assessment of ozone impacts on vegetation in the future, including: an increase in monitoring of ozone and collation of field evidence of the damaging effects on vegetation; an investigation of the effects on peri-urban agriculture and in mountain/upland areas; inclusion of additional pollutant, meteorological and inlet height data in the TOAR dataset; where not already in existence, establishing new region-specific thresholds for vegetation damage and an innovative integration of observations and modelling including stomatal uptake of the pollutant.
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskap0 (SwePub)1052 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciences0 (SwePub)1052 hsv//eng
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskapx Geologi0 (SwePub)105042 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Geology0 (SwePub)105042 hsv//eng
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskapx Naturgeografi0 (SwePub)105072 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Physical Geography0 (SwePub)105072 hsv//eng
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskapx Klimatforskning0 (SwePub)105012 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Climate Research0 (SwePub)105012 hsv//eng
653 a Ozone
653 a vegetation
653 a metrics
653 a crops
653 a perennials
653 a global
653 a dose-response relationships
653 a crop yield losses
653 a surface ozone
653 a united-states
653 a stomatal flux
653 a human health
653 a (semi-)natural vegetation
653 a primary productivity
653 a agricultural crops
653 a global impacts
653 a Environmental Sciences & Ecology
653 a Meteorology & Atmospheric Sciences
653 a Ozone
700a Pleijel, Håkan,d 1958u Gothenburg University,Göteborgs universitet,Institutionen för biologi och miljövetenskap,Department of Biological and Environmental Sciences,University of Gothenburg4 aut0 (Swepub:cth)xpleha
700a Malley, C. S.u University of Edinburgh,University of York,UK Centre For Ecology & Hydrology (UKCEH)4 aut
700a Sinha, B.u Indian Institute of Science4 aut
700a Cooper, O. R.u University of Colorado at Boulder4 aut
700a Schultz, M. G.u Forschungszentrum Jülich GmbH,Università Cattolica del Sacro Cuore4 aut
700a Neufeld, H. S.u Appalachian State University,UK Centre For Ecology & Hydrology (UKCEH)4 aut
700a Simpson, David,d 1961u Chalmers tekniska högskola,Chalmers University of Technology,Meteorologisk institutt,Norwegian Meteorological Institute4 aut0 (Swepub:cth)simpson
700a Sharps, K.u UK Centre For Ecology & Hydrology (UKCEH)4 aut
700a Feng, Z. Z.u Chinese Academy of Sciences4 aut
700a Gerosa, G.4 aut
700a Harmens, H.4 aut
700a Kobayashi, K.u University of Tokyo, Japan4 aut
700a Saxena, P.u Jawaharlal Nehru University4 aut
700a Paoletti, E.4 aut
700a Sinha, V.u Indian Institute of Science4 aut
700a Xu, X. B.u Chinese Academy of Meteorological Sciences (CAMS)4 aut
710a Göteborgs universitetb Institutionen för biologi och miljövetenskap4 org
773t Elementa-Science of the Anthropocened : University of California Pressg 6:1q 6:1x 2325-1026
856u https://doi.org/10.1525/elementa.302
856u https://research.chalmers.se/publication/505902/file/505902_Fulltext.pdfx primaryx freey FULLTEXT
8564 8u https://gup.ub.gu.se/publication/269046
8564 8u https://doi.org/10.1525/elementa.302
8564 8u https://research.chalmers.se/publication/505902

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