FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2104476525> ?p ?o ?g. }

• W2104476525 endingPage "10648" @default.
• W2104476525 startingPage "10633" @default.
• W2104476525 abstract "Abstract. Oceanic emissions of halogenated very short-lived substances (VSLS) are expected to contribute significantly to the stratospheric halogen loading and therefore to ozone depletion. The amount of VSLS transported into the stratosphere is estimated based on in-situ observations around the tropical tropopause layer (TTL) and on modeling studies which mostly use prescribed global emission scenarios to reproduce observed atmospheric concentrations. In addition to upper-air VSLS measurements, direct observations of oceanic VSLS emissions are available along ship cruise tracks. Here we use such in-situ observations of VSLS emissions from the West Pacific and tropical Atlantic together with an atmospheric Lagrangian transport model to estimate the direct contribution of bromoform (CHBr3), and dibromomethane (CH2Br2) to the stratospheric bromine loading as well as their ozone depletion potential. Our emission-based estimates of VSLS profiles are compared to upper-air observations and thus link observed oceanic emissions and in situ TTL measurements. This comparison determines how VSLS emissions and transport in the cruise track regions contribute to global upper-air VSLS estimates. The West Pacific emission-based profiles and the global upper-air observations of CHBr3 show a relatively good agreement indicating that emissions from the West Pacific provide an average contribution to the global CHBr3 budget. The tropical Atlantic, although also being a CHBr3 source region, is of less importance for global upper-air CHBr3 estimates as revealed by the small emission-based abundances in the TTL. Western Pacific CH2Br2 emission-based estimates are considerably smaller than upper-air observations as a result of the relatively low sea-to-air flux found in the West Pacific. Together, CHBr3 and CH2Br2 emissions from the West Pacific are projected to contribute to the stratospheric bromine budget with 0.4 pptv Br on average and 2.3 pptv Br for cases of maximum emissions through product and source gas injection. These relatively low estimates reveal that the tropical West Pacific, although characterized by strong convective transport, might overall contribute less VSLS to the stratospheric bromine budget than other regions as a result of only low CH2Br2 and moderate CHBr3 oceanic emissions." @default.
• W2104476525 created "2016-06-24" @default.
• W2104476525 creator A5009787481 @default.
• W2104476525 creator A5013391991 @default.
• W2104476525 creator A5024568254 @default.
• W2104476525 creator A5034645197 @default.
• W2104476525 creator A5047723373 @default.
• W2104476525 creator A5077376566 @default.
• W2104476525 creator A5088446807 @default.
• W2104476525 date "2012-11-16" @default.
• W2104476525 modified "2023-10-07" @default.
• W2104476525 title "Emission and transport of bromocarbons: from the West Pacific ocean into the stratosphere" @default.
• W2104476525 cites W1220726486 @default.
• W2104476525 cites W1484460586 @default.
• W2104476525 cites W1514104356 @default.
• W2104476525 cites W1964216405 @default.
• W2104476525 cites W1967823400 @default.
• W2104476525 cites W1968101284 @default.
• W2104476525 cites W1969544388 @default.
• W2104476525 cites W1986744491 @default.
• W2104476525 cites W1989957390 @default.
• W2104476525 cites W1995242642 @default.
• W2104476525 cites W1996376768 @default.
• W2104476525 cites W2000648149 @default.
• W2104476525 cites W2001450753 @default.
• W2104476525 cites W2009444488 @default.
• W2104476525 cites W2018750627 @default.
• W2104476525 cites W2023193957 @default.
• W2104476525 cites W2023502348 @default.
• W2104476525 cites W2036229814 @default.
• W2104476525 cites W2044331242 @default.
• W2104476525 cites W2044819502 @default.
• W2104476525 cites W2061609167 @default.
• W2104476525 cites W2061877440 @default.
• W2104476525 cites W2075281384 @default.
• W2104476525 cites W2076363916 @default.
• W2104476525 cites W2088156480 @default.
• W2104476525 cites W2090353819 @default.
• W2104476525 cites W2103399093 @default.
• W2104476525 cites W2104102313 @default.
• W2104476525 cites W2107023928 @default.
• W2104476525 cites W2107349299 @default.
• W2104476525 cites W2107725900 @default.
• W2104476525 cites W2108409370 @default.
• W2104476525 cites W2112684558 @default.
• W2104476525 cites W2113965453 @default.
• W2104476525 cites W2114212231 @default.
• W2104476525 cites W2117337967 @default.
• W2104476525 cites W2119021261 @default.
• W2104476525 cites W2121745948 @default.
• W2104476525 cites W2133755418 @default.
• W2104476525 cites W2135419069 @default.
• W2104476525 cites W2142522984 @default.
• W2104476525 cites W2142551124 @default.
• W2104476525 cites W2144185463 @default.
• W2104476525 cites W2147684755 @default.
• W2104476525 cites W2148028617 @default.
• W2104476525 cites W2149932227 @default.
• W2104476525 cites W2150360667 @default.
• W2104476525 cites W2150572267 @default.
• W2104476525 cites W2154943783 @default.
• W2104476525 cites W2156209025 @default.
• W2104476525 cites W2157494707 @default.
• W2104476525 cites W2158335488 @default.
• W2104476525 cites W2161345200 @default.
• W2104476525 cites W2163532696 @default.
• W2104476525 cites W2165217209 @default.
• W2104476525 cites W2165309387 @default.
• W2104476525 cites W2167894509 @default.
• W2104476525 cites W2169639098 @default.
• W2104476525 cites W2175515323 @default.
• W2104476525 cites W4206824192 @default.
• W2104476525 doi "https://doi.org/10.5194/acp-12-10633-2012" @default.
• W2104476525 hasPublicationYear "2012" @default.
• W2104476525 type Work @default.
• W2104476525 sameAs 2104476525 @default.
• W2104476525 citedByCount "62" @default.
• W2104476525 countsByYear W21044765252012 @default.
• W2104476525 countsByYear W21044765252013 @default.
• W2104476525 countsByYear W21044765252014 @default.
• W2104476525 countsByYear W21044765252015 @default.
• W2104476525 countsByYear W21044765252016 @default.
• W2104476525 countsByYear W21044765252017 @default.
• W2104476525 countsByYear W21044765252018 @default.
• W2104476525 countsByYear W21044765252019 @default.
• W2104476525 countsByYear W21044765252020 @default.
• W2104476525 countsByYear W21044765252021 @default.
• W2104476525 countsByYear W21044765252022 @default.
• W2104476525 countsByYear W21044765252023 @default.
• W2104476525 crossrefType "journal-article" @default.
• W2104476525 hasAuthorship W2104476525A5009787481 @default.
• W2104476525 hasAuthorship W2104476525A5013391991 @default.
• W2104476525 hasAuthorship W2104476525A5024568254 @default.
• W2104476525 hasAuthorship W2104476525A5034645197 @default.
• W2104476525 hasAuthorship W2104476525A5047723373 @default.
• W2104476525 hasAuthorship W2104476525A5077376566 @default.
• W2104476525 hasAuthorship W2104476525A5088446807 @default.
• W2104476525 hasBestOaLocation W21044765251 @default.

• next