FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2896900580> ?p ?o ?g. }

• W2896900580 endingPage "375" @default.
• W2896900580 startingPage "368" @default.
• W2896900580 abstract "Thanks to the Montreal Protocol, the stratospheric concentrations of ozone-depleting chlorine and bromine have been declining since their peak in the late 1990s. Global ozone has responded: The substantial ozone decline observed since the 1960s ended in the late 1990s. Since then, ozone levels have remained low, but have not declined further. Now general ozone increases and a slow recovery of the ozone layer is expected. The clearest signs of increasing ozone, so far, are seen in the upper stratosphere and for total ozone columns above Antarctica in spring. These two regions had also seen the largest ozone depletions in the past. Total column ozone at most latitudes, however, does not show clear increases yet. This is not unexpected, because the removal of chlorine and bromine from the stratosphere is three to four times slower than their previous increase. Detecting significant increases in total column ozone, therefore, will require much more time than the detection of its previous decline. The search is complicated by variations in ozone that are not caused by declining chlorine or bromine, but are due, e.g., to transport changes in the global Brewer–Dobson circulation. Also, very accurate observations are necessary to detect the expected small increases. Nevertheless, observations and model simulations indicate that the stratosphere is on the path to ozone recovery. This recovery process will take many decades. As chlorine and bromine decline, other factors will become more important. These include climate change and its effects on stratospheric temperatures, changes in the Brewer–Dobson circulation (both due to increasing CO2), increasing emissions of trace gases like N2O, CH4, possibly large future increases of short-lived substances (like CCl2H2) from both natural and anthropogenic sources, and changes in tropospheric ozone." @default.
• W2896900580 created "2018-10-26" @default.
• W2896900580 creator A5010850538 @default.
• W2896900580 creator A5038838249 @default.
• W2896900580 creator A5060394551 @default.
• W2896900580 creator A5061379765 @default.
• W2896900580 date "2018-11-01" @default.
• W2896900580 modified "2023-10-16" @default.
• W2896900580 title "Is global ozone recovering?" @default.
• W2896900580 cites W1966733172 @default.
• W2896900580 cites W1981052127 @default.
• W2896900580 cites W1987770728 @default.
• W2896900580 cites W1992227592 @default.
• W2896900580 cites W2016265957 @default.
• W2896900580 cites W2046561232 @default.
• W2896900580 cites W2066342707 @default.
• W2896900580 cites W2070109551 @default.
• W2896900580 cites W2072298480 @default.
• W2896900580 cites W2081773255 @default.
• W2896900580 cites W2103381339 @default.
• W2896900580 cites W2104441266 @default.
• W2896900580 cites W2122060346 @default.
• W2896900580 cites W2122629187 @default.
• W2896900580 cites W2131598229 @default.
• W2896900580 cites W2131696721 @default.
• W2896900580 cites W2134464340 @default.
• W2896900580 cites W2135334119 @default.
• W2896900580 cites W2147382978 @default.
• W2896900580 cites W2148717919 @default.
• W2896900580 cites W2155647793 @default.
• W2896900580 cites W2156092764 @default.
• W2896900580 cites W2156808923 @default.
• W2896900580 cites W2345816956 @default.
• W2896900580 cites W2405563765 @default.
• W2896900580 cites W2468673805 @default.
• W2896900580 cites W2588353936 @default.
• W2896900580 cites W2611933393 @default.
• W2896900580 cites W2621982623 @default.
• W2896900580 cites W2689918507 @default.
• W2896900580 cites W2734190852 @default.
• W2896900580 cites W2740188812 @default.
• W2896900580 cites W2748511849 @default.
• W2896900580 cites W2754901818 @default.
• W2896900580 cites W2754904600 @default.
• W2896900580 cites W2762229760 @default.
• W2896900580 cites W2769762907 @default.
• W2896900580 cites W2773678058 @default.
• W2896900580 cites W2786941826 @default.
• W2896900580 doi "https://doi.org/10.1016/j.crte.2018.07.012" @default.
• W2896900580 hasPublicationYear "2018" @default.
• W2896900580 type Work @default.
• W2896900580 sameAs 2896900580 @default.
• W2896900580 citedByCount "26" @default.
• W2896900580 countsByYear W28969005802019 @default.
• W2896900580 countsByYear W28969005802020 @default.
• W2896900580 countsByYear W28969005802021 @default.
• W2896900580 countsByYear W28969005802022 @default.
• W2896900580 countsByYear W28969005802023 @default.
• W2896900580 crossrefType "journal-article" @default.
• W2896900580 hasAuthorship W2896900580A5010850538 @default.
• W2896900580 hasAuthorship W2896900580A5038838249 @default.
• W2896900580 hasAuthorship W2896900580A5060394551 @default.
• W2896900580 hasAuthorship W2896900580A5061379765 @default.
• W2896900580 hasBestOaLocation W28969005801 @default.
• W2896900580 hasConcept C115719804 @default.
• W2896900580 hasConcept C122523270 @default.
• W2896900580 hasConcept C127313418 @default.
• W2896900580 hasConcept C13280743 @default.
• W2896900580 hasConcept C141810719 @default.
• W2896900580 hasConcept C153294291 @default.
• W2896900580 hasConcept C163861444 @default.
• W2896900580 hasConcept C178790620 @default.
• W2896900580 hasConcept C185592680 @default.
• W2896900580 hasConcept C205649164 @default.
• W2896900580 hasConcept C2777677027 @default.
• W2896900580 hasConcept C39432304 @default.
• W2896900580 hasConcept C49204034 @default.
• W2896900580 hasConcept C505241676 @default.
• W2896900580 hasConcept C508106653 @default.
• W2896900580 hasConcept C517835270 @default.
• W2896900580 hasConcept C91586092 @default.
• W2896900580 hasConceptScore W2896900580C115719804 @default.
• W2896900580 hasConceptScore W2896900580C122523270 @default.
• W2896900580 hasConceptScore W2896900580C127313418 @default.
• W2896900580 hasConceptScore W2896900580C13280743 @default.
• W2896900580 hasConceptScore W2896900580C141810719 @default.
• W2896900580 hasConceptScore W2896900580C153294291 @default.
• W2896900580 hasConceptScore W2896900580C163861444 @default.
• W2896900580 hasConceptScore W2896900580C178790620 @default.
• W2896900580 hasConceptScore W2896900580C185592680 @default.
• W2896900580 hasConceptScore W2896900580C205649164 @default.
• W2896900580 hasConceptScore W2896900580C2777677027 @default.
• W2896900580 hasConceptScore W2896900580C39432304 @default.
• W2896900580 hasConceptScore W2896900580C49204034 @default.
• W2896900580 hasConceptScore W2896900580C505241676 @default.
• W2896900580 hasConceptScore W2896900580C508106653 @default.
• W2896900580 hasConceptScore W2896900580C517835270 @default.
• W2896900580 hasConceptScore W2896900580C91586092 @default.

• next