Matches in SemOpenAlex for { <https://semopenalex.org/work/W2004380096> ?p ?o ?g. }
- W2004380096 endingPage "3442" @default.
- W2004380096 startingPage "3431" @default.
- W2004380096 abstract "A survey of the literature was conducted to review historical and current surface ozone data from background stations in Canada, United States and around the world for the purpose of characterizing background levels and trends, present plausible explanations for observed trends and explore projections of future ozone levels. The annual ozone cycle at background sites in the Northern Hemisphere is characterized by a spring maximum, peaking during the month of May. Although presently there is no concensus as to the origin of the spring maximum, evidence supports both enhanced photochemistry in the free troposphere and stratospheric input. Modern day annual average background ozone concentrations over the midlatitudes of the Northern Hemisphere range between approximately 20–45 ppb, with variability being a function of geographic location, elevation and extent of anthropogenic influence. Annual median ozone levels at Canadian background stations fall between 23 and 34 ppb, a range similar to that reported for low-elevation background stations in the United States and around the world. Comparisons of ozone levels with those measured over a century ago indicate that current levels have increased by approximately two times. Although current trends are not uniform, there is some indication that background ozone levels over the midlatitudes of the Northern Hemisphere have continued to rise over the past three decades, and that this rise has been in the range of approximately 0.5–2% per year. Rising trends were steeper in the 1970s and 1980s compared to the 1990s, which have seen either a leveling off or a decline in the magnitude of these trends. Model sensitivity studies indicate that the rise in NOx emissions account for the greatest increase in background ozone levels over the past three decades. A substantial component of the background ozone concentration in western North America may be due to long-range transport of Asian pollution, especially during the spring months. Model projections using IPCC emission scenarios for the 21st century indicate that background ozone may rise to levels that would exceed internationally accepted environmental criteria for human health and the environment." @default.
- W2004380096 created "2016-06-24" @default.
- W2004380096 creator A5063939478 @default.
- W2004380096 date "2004-07-01" @default.
- W2004380096 modified "2023-10-10" @default.
- W2004380096 title "A review of surface ozone background levels and trends" @default.
- W2004380096 cites W103794314 @default.
- W2004380096 cites W1522296012 @default.
- W2004380096 cites W1542477452 @default.
- W2004380096 cites W1579933083 @default.
- W2004380096 cites W1590695593 @default.
- W2004380096 cites W1607406231 @default.
- W2004380096 cites W178270748 @default.
- W2004380096 cites W1965249271 @default.
- W2004380096 cites W1966561125 @default.
- W2004380096 cites W1967408391 @default.
- W2004380096 cites W1967551491 @default.
- W2004380096 cites W1968887002 @default.
- W2004380096 cites W1969834329 @default.
- W2004380096 cites W1971494184 @default.
- W2004380096 cites W1978477930 @default.
- W2004380096 cites W1978855535 @default.
- W2004380096 cites W1980844880 @default.
- W2004380096 cites W1986127040 @default.
- W2004380096 cites W1988526495 @default.
- W2004380096 cites W1989228002 @default.
- W2004380096 cites W1995128882 @default.
- W2004380096 cites W2001451142 @default.
- W2004380096 cites W2003424948 @default.
- W2004380096 cites W2008046036 @default.
- W2004380096 cites W2013214260 @default.
- W2004380096 cites W2014944097 @default.
- W2004380096 cites W2017585288 @default.
- W2004380096 cites W2020100832 @default.
- W2004380096 cites W2020147105 @default.
- W2004380096 cites W2024626134 @default.
- W2004380096 cites W2025259712 @default.
- W2004380096 cites W2025646674 @default.
- W2004380096 cites W2028179607 @default.
- W2004380096 cites W2029688439 @default.
- W2004380096 cites W2030005508 @default.
- W2004380096 cites W2033803435 @default.
- W2004380096 cites W2035050838 @default.
- W2004380096 cites W2038254493 @default.
- W2004380096 cites W2045098694 @default.
- W2004380096 cites W2053566754 @default.
- W2004380096 cites W2061614887 @default.
- W2004380096 cites W2062667641 @default.
- W2004380096 cites W2066172543 @default.
- W2004380096 cites W2066826653 @default.
- W2004380096 cites W2072252541 @default.
- W2004380096 cites W2072489060 @default.
- W2004380096 cites W2073002771 @default.
- W2004380096 cites W2073028483 @default.
- W2004380096 cites W2073104487 @default.
- W2004380096 cites W2073330111 @default.
- W2004380096 cites W2074912331 @default.
- W2004380096 cites W2075281384 @default.
- W2004380096 cites W2075525816 @default.
- W2004380096 cites W2079217415 @default.
- W2004380096 cites W2082443156 @default.
- W2004380096 cites W2085109789 @default.
- W2004380096 cites W2089657057 @default.
- W2004380096 cites W2091269135 @default.
- W2004380096 cites W2092928991 @default.
- W2004380096 cites W2100748603 @default.
- W2004380096 cites W2102303629 @default.
- W2004380096 cites W2144475649 @default.
- W2004380096 cites W2152659471 @default.
- W2004380096 cites W2156929172 @default.
- W2004380096 cites W2165708514 @default.
- W2004380096 cites W2167505811 @default.
- W2004380096 cites W2169640928 @default.
- W2004380096 cites W2171204536 @default.
- W2004380096 cites W2312753739 @default.
- W2004380096 cites W265920339 @default.
- W2004380096 cites W268092627 @default.
- W2004380096 cites W3125900351 @default.
- W2004380096 cites W91256079 @default.
- W2004380096 cites W2613437875 @default.
- W2004380096 doi "https://doi.org/10.1016/j.atmosenv.2004.03.030" @default.
- W2004380096 hasPublicationYear "2004" @default.
- W2004380096 type Work @default.
- W2004380096 sameAs 2004380096 @default.
- W2004380096 citedByCount "1034" @default.
- W2004380096 countsByYear W20043800962012 @default.
- W2004380096 countsByYear W20043800962013 @default.
- W2004380096 countsByYear W20043800962014 @default.
- W2004380096 countsByYear W20043800962015 @default.
- W2004380096 countsByYear W20043800962016 @default.
- W2004380096 countsByYear W20043800962017 @default.
- W2004380096 countsByYear W20043800962018 @default.
- W2004380096 countsByYear W20043800962019 @default.
- W2004380096 countsByYear W20043800962020 @default.
- W2004380096 countsByYear W20043800962021 @default.
- W2004380096 countsByYear W20043800962022 @default.
- W2004380096 countsByYear W20043800962023 @default.
- W2004380096 crossrefType "journal-article" @default.