FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4229071771> ?p ?o ?g. }

• W4229071771 abstract "This study presents an updated evaluation of stratospheric ozone profile trends in the 60° S–60° N latitude range over the 2000–2020 period, using an updated version of the Long-term Ozone Trends and Uncertainties in the Stratosphere (LOTUS) regression model that was used to evaluate such trends up to 2016 for the last WMO Ozone Assessment (2018). In addition to the derivation of detailed trends as a function of latitude and vertical coordinates, the regressions are performed with the data sets averaged over broad latitude bands, i.e. 60° S–35° S, 20° S–20° N and 35° N–60° N. The same methodology as in the last Assessment is applied to combine trends in these broad latitude bands in order to compare the results with the previous studies. Longitudinally resolved merged satellite records are also considered in order to provide a better comparison with trends retrieved from ground-based records, e.g. lidar, ozone sondes, Umkehr, microwave and Fourier Transform Infrared (FTIR) spectrometers at selected stations where long-term time series are available. The study includes a comparison with trends derived from the latest REF-C2 simulations of the Chemistry Climate Model Initiative (CCMI). This work confirms past results showing an ozone increase in the upper stratosphere, which is now significant in the three broad latitude bands. The increase is largest in the northern and southern hemisphere midlatitudes, with ~2.2 %/decade at ~2.1 hPa, and ~2.1 %/decade at ~3.2 hPa respectively, compared to ~1.6 %/decade at ~2.6 hPa in the tropics. New trend signals have emerged from the records, such as a significant decrease of ozone in the tropics around 35 hPa and a non-significant increase of ozone in the southern mid-latitudes at about 20 hPa. Non-significant negative ozone trends are derived in the lowermost stratosphere, with the most pronounced trends in the tropics. While a very good agreement is obtained between trends from merged satellite records and the CCMI REF-C2 simulation in the upper stratosphere, observed negative trends in the lower stratosphere are not reproduced by models at southern and, in particular, at northern midlatitudes, where models report an ozone increase. However, the lower stratospheric trend uncertainties are quite large, for both measured and modelled trends. Finally, 2000–2020 stratospheric ozone trends derived from the ground-based and longitudinally resolved satellite records are in close agreement, especially over the European Alpine and tropical regions." @default.
• W4229071771 created "2022-05-08" @default.
• W4229071771 creator A5031901270 @default.
• W4229071771 date "2022-05-05" @default.
• W4229071771 modified "2023-10-01" @default.
• W4229071771 title "Reply on CC1" @default.
• W4229071771 doi "https://doi.org/10.5194/acp-2022-137-ac3" @default.
• W4229071771 hasPublicationYear "2022" @default.
• W4229071771 type Work @default.
• W4229071771 citedByCount "0" @default.
• W4229071771 crossrefType "peer-review" @default.
• W4229071771 hasAuthorship W4229071771A5031901270 @default.
• W4229071771 hasBestOaLocation W42290717711 @default.
• W4229071771 hasConcept C121332964 @default.
• W4229071771 hasConcept C122523270 @default.
• W4229071771 hasConcept C127313418 @default.
• W4229071771 hasConcept C1276947 @default.
• W4229071771 hasConcept C13280743 @default.
• W4229071771 hasConcept C141810719 @default.
• W4229071771 hasConcept C153294291 @default.
• W4229071771 hasConcept C163861444 @default.
• W4229071771 hasConcept C18101618 @default.
• W4229071771 hasConcept C19269812 @default.
• W4229071771 hasConcept C205649164 @default.
• W4229071771 hasConcept C2777252438 @default.
• W4229071771 hasConcept C2778835443 @default.
• W4229071771 hasConcept C39432304 @default.
• W4229071771 hasConcept C49204034 @default.
• W4229071771 hasConcept C508106653 @default.
• W4229071771 hasConcept C91586092 @default.
• W4229071771 hasConceptScore W4229071771C121332964 @default.
• W4229071771 hasConceptScore W4229071771C122523270 @default.
• W4229071771 hasConceptScore W4229071771C127313418 @default.
• W4229071771 hasConceptScore W4229071771C1276947 @default.
• W4229071771 hasConceptScore W4229071771C13280743 @default.
• W4229071771 hasConceptScore W4229071771C141810719 @default.
• W4229071771 hasConceptScore W4229071771C153294291 @default.
• W4229071771 hasConceptScore W4229071771C163861444 @default.
• W4229071771 hasConceptScore W4229071771C18101618 @default.
• W4229071771 hasConceptScore W4229071771C19269812 @default.
• W4229071771 hasConceptScore W4229071771C205649164 @default.
• W4229071771 hasConceptScore W4229071771C2777252438 @default.
• W4229071771 hasConceptScore W4229071771C2778835443 @default.
• W4229071771 hasConceptScore W4229071771C39432304 @default.
• W4229071771 hasConceptScore W4229071771C49204034 @default.
• W4229071771 hasConceptScore W4229071771C508106653 @default.
• W4229071771 hasConceptScore W4229071771C91586092 @default.
• W4229071771 hasLocation W42290717711 @default.
• W4229071771 hasOpenAccess W4229071771 @default.
• W4229071771 hasPrimaryLocation W42290717711 @default.
• W4229071771 hasRelatedWork W1972148312 @default.
• W4229071771 hasRelatedWork W1977489501 @default.
• W4229071771 hasRelatedWork W1986775482 @default.
• W4229071771 hasRelatedWork W1994617455 @default.
• W4229071771 hasRelatedWork W2168841033 @default.
• W4229071771 hasRelatedWork W2302020500 @default.
• W4229071771 hasRelatedWork W4249890833 @default.
• W4229071771 hasRelatedWork W4253395781 @default.
• W4229071771 hasRelatedWork W4320032030 @default.
• W4229071771 hasRelatedWork W821273240 @default.
• W4229071771 isParatext "false" @default.
• W4229071771 isRetracted "false" @default.
• W4229071771 workType "peer-review" @default.