FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3032059635> ?p ?o ?g. }

• W3032059635 abstract "Abstract Two decades into the 21st century there is growing evidence for global impacts of Antarctic and Southern Ocean climate change. Reliable estimates of how the Antarctic climate system would behave under a range of scenarios of future external climate forcing are thus a high priority. Output from new model simulations coordinated as part of the Coupled Model Intercomparison Project Phase 6 (CMIP6) provides an opportunity for a comprehensive analysis of the latest generation of state‐of‐the‐art climate models following a wider range of experiment types and scenarios than previous CMIP phases. Here the main broad‐scale 21st century Antarctic projections provided by the CMIP6 models are shown across four forcing scenarios: SSP1‐2.6, SSP2‐4.5, SSP3‐7.0 and SSP5‐8.5. End‐of‐century Antarctic surface‐air temperature change across these scenarios (relative to 1995–2014) is 1.3, 2.5, 3.7 and 4.8°C. The corresponding proportional precipitation rate changes are 8, 16, 24 and 31%. In addition to these end‐of‐century changes, an assessment of scenario dependence of pathways of absolute and global‐relative 21st century projections is conducted. Potential differences in regional response are of particular relevance to coastal Antarctica, where, for example, ecosystems and ice shelves are highly sensitive to the timing of crossing of key thresholds in both atmospheric and oceanic conditions. Overall, it is found that the projected changes over coastal Antarctica do not scale linearly with global forcing. We identify two factors that appear to contribute: (a) a stronger global‐relative Southern Ocean warming in stabilisation (SSP2‐4.5) and aggressive mitigation (SSP1‐2.6) scenarios as the Southern Ocean continues to warm and (b) projected recovery of Southern Hemisphere stratospheric ozone and its effect on the mid‐latitude westerlies. The major implication is that over coastal Antarctica, the surface warming by 2100 is stronger relative to the global mean surface warming for the low forcing compared to high forcing future scenarios." @default.
• W3032059635 created "2020-06-05" @default.
• W3032059635 creator A5007268175 @default.
• W3032059635 creator A5021631028 @default.
• W3032059635 creator A5023021312 @default.
• W3032059635 creator A5023159094 @default.
• W3032059635 creator A5037577056 @default.
• W3032059635 creator A5052568750 @default.
• W3032059635 creator A5067037702 @default.
• W3032059635 creator A5083877119 @default.
• W3032059635 date "2020-05-28" @default.
• W3032059635 modified "2023-10-16" @default.
• W3032059635 title "Twenty first century changes in Antarctic and Southern Ocean surface climate in CMIP6" @default.
• W3032059635 cites W1974010481 @default.
• W3032059635 cites W1994149669 @default.
• W3032059635 cites W2018247270 @default.
• W3032059635 cites W2024966118 @default.
• W3032059635 cites W2051761224 @default.
• W3032059635 cites W2053162006 @default.
• W3032059635 cites W2054874891 @default.
• W3032059635 cites W2070886035 @default.
• W3032059635 cites W2072772553 @default.
• W3032059635 cites W2080192596 @default.
• W3032059635 cites W2100913382 @default.
• W3032059635 cites W2133606218 @default.
• W3032059635 cites W2151244793 @default.
• W3032059635 cites W2156309025 @default.
• W3032059635 cites W2157087879 @default.
• W3032059635 cites W2170418996 @default.
• W3032059635 cites W2171984413 @default.
• W3032059635 cites W2193503481 @default.
• W3032059635 cites W2256787008 @default.
• W3032059635 cites W2318888902 @default.
• W3032059635 cites W2320249130 @default.
• W3032059635 cites W2337225114 @default.
• W3032059635 cites W2409662752 @default.
• W3032059635 cites W2480261700 @default.
• W3032059635 cites W2564171595 @default.
• W3032059635 cites W2587774659 @default.
• W3032059635 cites W2725707462 @default.
• W3032059635 cites W2741413404 @default.
• W3032059635 cites W2748442592 @default.
• W3032059635 cites W2755648354 @default.
• W3032059635 cites W2787362345 @default.
• W3032059635 cites W2803704702 @default.
• W3032059635 cites W2807097649 @default.
• W3032059635 cites W2901463946 @default.
• W3032059635 cites W2902834734 @default.
• W3032059635 cites W2904441986 @default.
• W3032059635 cites W2914023611 @default.
• W3032059635 cites W2915006888 @default.
• W3032059635 cites W2922127343 @default.
• W3032059635 cites W2981859133 @default.
• W3032059635 cites W2983748618 @default.
• W3032059635 doi "https://doi.org/10.1002/asl.984" @default.
• W3032059635 hasPublicationYear "2020" @default.
• W3032059635 type Work @default.
• W3032059635 sameAs 3032059635 @default.
• W3032059635 citedByCount "47" @default.
• W3032059635 countsByYear W30320596352020 @default.
• W3032059635 countsByYear W30320596352021 @default.
• W3032059635 countsByYear W30320596352022 @default.
• W3032059635 countsByYear W30320596352023 @default.
• W3032059635 crossrefType "journal-article" @default.
• W3032059635 hasAuthorship W3032059635A5007268175 @default.
• W3032059635 hasAuthorship W3032059635A5021631028 @default.
• W3032059635 hasAuthorship W3032059635A5023021312 @default.
• W3032059635 hasAuthorship W3032059635A5023159094 @default.
• W3032059635 hasAuthorship W3032059635A5037577056 @default.
• W3032059635 hasAuthorship W3032059635A5052568750 @default.
• W3032059635 hasAuthorship W3032059635A5067037702 @default.
• W3032059635 hasAuthorship W3032059635A5083877119 @default.
• W3032059635 hasBestOaLocation W30320596351 @default.
• W3032059635 hasConcept C107054158 @default.
• W3032059635 hasConcept C111368507 @default.
• W3032059635 hasConcept C127313418 @default.
• W3032059635 hasConcept C132651083 @default.
• W3032059635 hasConcept C153294291 @default.
• W3032059635 hasConcept C159985019 @default.
• W3032059635 hasConcept C168754636 @default.
• W3032059635 hasConcept C192562407 @default.
• W3032059635 hasConcept C197115733 @default.
• W3032059635 hasConcept C199491958 @default.
• W3032059635 hasConcept C204323151 @default.
• W3032059635 hasConcept C205649164 @default.
• W3032059635 hasConcept C25022447 @default.
• W3032059635 hasConcept C39432304 @default.
• W3032059635 hasConcept C49204034 @default.
• W3032059635 hasConcept C99578197 @default.
• W3032059635 hasConceptScore W3032059635C107054158 @default.
• W3032059635 hasConceptScore W3032059635C111368507 @default.
• W3032059635 hasConceptScore W3032059635C127313418 @default.
• W3032059635 hasConceptScore W3032059635C132651083 @default.
• W3032059635 hasConceptScore W3032059635C153294291 @default.
• W3032059635 hasConceptScore W3032059635C159985019 @default.
• W3032059635 hasConceptScore W3032059635C168754636 @default.
• W3032059635 hasConceptScore W3032059635C192562407 @default.
• W3032059635 hasConceptScore W3032059635C197115733 @default.
• W3032059635 hasConceptScore W3032059635C199491958 @default.
• W3032059635 hasConceptScore W3032059635C204323151 @default.

• next