FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1986945118> ?p ?o ?g. }

• W1986945118 endingPage "518" @default.
• W1986945118 startingPage "497" @default.
• W1986945118 abstract "Atmospheric trace gas studies in Antarctica have led to an increased understanding of the global effects from anthropogenic emissions of various compounds. These studies have also contributed to the identification of various atmospheric circulation patterns and mixing mechanisms. Time trend analyses have revealed that although the atmospheric concentrations of F‐11, F‐12, CH 3 CCl 3 , and other halocarbons are still increasing, their rate of increase has slowed from peak increasing rates observed in the 1970s. For CO 2 , CO, and CH 4 , time trend analyses have also been used to analyze seasonal concentration cycles and to establish relationships between sources and sinks at various times throughout the year. Latitudinal gradient studies have generally revealed that for most compounds with significant anthropogenic sources, atmospheric concentrations are higher in the northern hemisphere than in the southern hemisphere. This is mainly a result of the overwhelming majority of anthropogenic sources existing in the northern hemisphere. Vertical concentration profiles in Antarctica are dependent upon the seasonal variations in circulation patterns associated with final warming and breakup of the polar vortex. Since final warming and breakup of the polar vortex may not always occur at the same time each year, profiles for a given time period from separate years may be different. Stratospheric‐tropospheric air exchange over Antarctica occurs primarily as a result of (1) general circulation patterns with subsidence over the polar regions, (2) stratospheric air injection in the vicinity of jet streams and injection from tropopause folding upstream of troughs, and (3) mountain waves of sufficient magnitude to displace air parcels across the tropopause." @default.
• W1986945118 created "2016-06-24" @default.
• W1986945118 creator A5055564029 @default.
• W1986945118 creator A5063886575 @default.
• W1986945118 date "1988-08-01" @default.
• W1986945118 modified "2023-09-27" @default.
• W1986945118 title "Atmospheric trace gas studies in Antarctica" @default.
• W1986945118 cites W1945233050 @default.
• W1986945118 cites W1966786574 @default.
• W1986945118 cites W1967953223 @default.
• W1986945118 cites W1971438331 @default.
• W1986945118 cites W1971991115 @default.
• W1986945118 cites W1974406083 @default.
• W1986945118 cites W1976241928 @default.
• W1986945118 cites W1976870655 @default.
• W1986945118 cites W1977224850 @default.
• W1986945118 cites W1979199890 @default.
• W1986945118 cites W1984682613 @default.
• W1986945118 cites W1985462987 @default.
• W1986945118 cites W1985805045 @default.
• W1986945118 cites W1986565195 @default.
• W1986945118 cites W1994151189 @default.
• W1986945118 cites W1995199709 @default.
• W1986945118 cites W1998619483 @default.
• W1986945118 cites W2001147173 @default.
• W1986945118 cites W2001380745 @default.
• W1986945118 cites W2001551338 @default.
• W1986945118 cites W2002082344 @default.
• W1986945118 cites W2004405436 @default.
• W1986945118 cites W2006228910 @default.
• W1986945118 cites W2010043247 @default.
• W1986945118 cites W2014305081 @default.
• W1986945118 cites W2014471711 @default.
• W1986945118 cites W2014711847 @default.
• W1986945118 cites W2017262495 @default.
• W1986945118 cites W2017699035 @default.
• W1986945118 cites W2020240498 @default.
• W1986945118 cites W2020965636 @default.
• W1986945118 cites W2023820439 @default.
• W1986945118 cites W2025277953 @default.
• W1986945118 cites W2026522642 @default.
• W1986945118 cites W2036277636 @default.
• W1986945118 cites W2040888133 @default.
• W1986945118 cites W2043591064 @default.
• W1986945118 cites W2044467119 @default.
• W1986945118 cites W2047514174 @default.
• W1986945118 cites W2047756866 @default.
• W1986945118 cites W2051701872 @default.
• W1986945118 cites W2052707460 @default.
• W1986945118 cites W2055698954 @default.
• W1986945118 cites W2057236361 @default.
• W1986945118 cites W2058179313 @default.
• W1986945118 cites W2061059146 @default.
• W1986945118 cites W2064426298 @default.
• W1986945118 cites W2066194063 @default.
• W1986945118 cites W2067184883 @default.
• W1986945118 cites W2068562247 @default.
• W1986945118 cites W2069457314 @default.
• W1986945118 cites W2070442118 @default.
• W1986945118 cites W2073159244 @default.
• W1986945118 cites W2074425650 @default.
• W1986945118 cites W2076363916 @default.
• W1986945118 cites W2078418089 @default.
• W1986945118 cites W2079762204 @default.
• W1986945118 cites W2084491032 @default.
• W1986945118 cites W2085259797 @default.
• W1986945118 cites W2087467202 @default.
• W1986945118 cites W2094841197 @default.
• W1986945118 cites W2096838487 @default.
• W1986945118 cites W2104307324 @default.
• W1986945118 cites W2114143316 @default.
• W1986945118 cites W2126774210 @default.
• W1986945118 cites W2142258967 @default.
• W1986945118 cites W2147243326 @default.
• W1986945118 cites W2156497406 @default.
• W1986945118 cites W2163336019 @default.
• W1986945118 cites W2166620677 @default.
• W1986945118 cites W2174335611 @default.
• W1986945118 cites W4231729316 @default.
• W1986945118 cites W4238581622 @default.
• W1986945118 cites W4241342624 @default.
• W1986945118 cites W4243031716 @default.
• W1986945118 doi "https://doi.org/10.1029/rg026i003p00497" @default.
• W1986945118 hasPublicationYear "1988" @default.
• W1986945118 type Work @default.
• W1986945118 sameAs 1986945118 @default.
• W1986945118 citedByCount "5" @default.
• W1986945118 crossrefType "journal-article" @default.
• W1986945118 hasAuthorship W1986945118A5055564029 @default.
• W1986945118 hasAuthorship W1986945118A5063886575 @default.
• W1986945118 hasConcept C109007969 @default.
• W1986945118 hasConcept C114793014 @default.
• W1986945118 hasConcept C119947313 @default.
• W1986945118 hasConcept C121332964 @default.
• W1986945118 hasConcept C125405218 @default.
• W1986945118 hasConcept C127313418 @default.
• W1986945118 hasConcept C130047971 @default.
• W1986945118 hasConcept C150284090 @default.

• next