Zobrazeno 1 - 10
of 42
pro vyhledávání: '"Paulo Ceppi"'
Autor:
Johannes Quaas, Timothy Andrews, Nicolas Bellouin, Karoline Block, Olivier Boucher, Paulo Ceppi, Guy Dagan, Sabine Doktorowski, Hannah Marie Eichholz, Piers Forster, Tom Goren, Edward Gryspeerdt, Øivind Hodnebrog, Hailing Jia, Ryan Kramer, Charlotte Lange, Amanda C. Maycock, Johannes Mülmenstädt, Gunnar Myhre, Fiona M. O’Connor, Robert Pincus, Bjørn Hallvard Samset, Fabian Senf, Keith P. Shine, Chris Smith, Camilla Weum Stjern, Toshihiko Takemura, Velle Toll, Casey J. Wall
Publikováno v:
AGU Advances, Vol 5, Iss 5, Pp n/a-n/a (2024)
Abstract Since the 5th Assessment Report of the Intergovernmental Panel on Climate Change (AR5) an extended concept of the energetic analysis of climate change including forcings, feedbacks and adjustment processes has become widely adopted. Adjustme
Externí odkaz:
https://doaj.org/article/e04dc6dd42fe4d4bad3e70c5b98e9c6a
Publikováno v:
Environmental Research Letters, Vol 15, Iss 9, p 0940c1 (2020)
The surface warming response to carbon emissions is diagnosed using a suite of Earth system models, 9 CMIP6 and 7 CMIP5, following an annual 1% rise in atmospheric CO _2 over 140 years. This surface warming response defines a climate metric, the Tran
Externí odkaz:
https://doaj.org/article/1de803d5118d4c62ac60889108c2e2fb
Publikováno v:
Environmental Research Letters, Vol 15, Iss 6, p 064011 (2020)
Global climate models indicate that the Southern Hemispheric (SH) jet stream shifts poleward in response to CO _2 forcing, but the magnitude of this shift remains highly uncertain. Here we analyse the SH jet stream response to 4×CO _2 forcing in Cou
Externí odkaz:
https://doaj.org/article/facb9ca8a78647e09f6fbe8c5fd31bf3
Data for the paper "Recent global climate feedback controlled by Southern Ocean cooling". The CESM2's Southern Ocean pacemaker experiment (SOPACE2)data for the analysis is uploaded as mat (matlab data format) files. In addition, the CESM2's Green's f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3deabff499e84e0a0757b1d0335c2b97
The effect of the Southern Ocean on global climate change is assessed using Earth system model projections following an idealized 1% annual rise in atmospheric CO 2 . For this scenario, the Southern Ocean plays a significant role in sequestering heat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::89baf02ffc667f3fa21283948f622b84
https://royalsocietypublishing.org/doi/full/10.1098/rsta.2022.0062
https://royalsocietypublishing.org/doi/full/10.1098/rsta.2022.0062
Autor:
Peer Nowack, Paulo Ceppi, Sean Davis, Gabriel Chiodo, Will Ball, Mohamadou A. Diallo, Birgit Hassler, Yue Jia, James Keeble, Manoj Joshi
Future increases in stratospheric water vapour (SWV) risk amplifying climate change and slowing down the recovery of the ozone layer. However, state-of-the-art climate models strongly disagree on the magnitude of these increases under global warming1
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::324707d514f3ae4491a3030695ec86c2
https://doi.org/10.5194/egusphere-egu23-2943
https://doi.org/10.5194/egusphere-egu23-2943
Most climate models show a poleward shift of the southern hemispheric zonal-mean jet in response to climate change, but the inter-model spread is large. In an attempt to constrain future jet responses, past studies have identified an emergent constra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::06182af2dd274eaf78b6d73bf5d81c0a
https://doi.org/10.5194/wcd-2022-42
https://doi.org/10.5194/wcd-2022-42
Climate models show a wide range of southern hemispheric jet responses to greenhouse gas forcing. One approach to constrain the future jet response is by utilising the fluctuation–dissipation theorem (FDT) which links the forced response to interna
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::420bb1a01760190f59292dffd634825f
http://hdl.handle.net/10044/1/99907
http://hdl.handle.net/10044/1/99907
Experiments with seven Coupled Model Intercomparison Project phase 6 models were used to assess the climate feedback parameter for net historical, historical greenhouse gas (GHG) and anthropogenic aerosol forcings. The net radiative feedback is found
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e0079a0bf463d443f4734c4452e438d4
http://hdl.handle.net/10044/1/99909
http://hdl.handle.net/10044/1/99909
Effective radiative forcing includes a contribution by rapid adjustments, i.e. changes in temperature, water vapour and clouds that modify the energy budget. Cloud adjustments in particular have been shown to depend strongly on forcing agent. We perf
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::abb66ec1120cabd9a8fc0bf0346d1f80
https://centaur.reading.ac.uk/99940/8/2021GL093616.pdf
https://centaur.reading.ac.uk/99940/8/2021GL093616.pdf