Zobrazeno 1 - 10
of 28
pro vyhledávání: '"Pepijn Bakker"'
Autor:
OLGA EROKHINA, IRINA ROGOZHINA, MATTHIAS PRANGE, PEPIJN BAKKER, JORGE BERNALES, ANDRÉ PAUL, MICHAEL SCHULZ
Publikováno v:
Journal of Glaciology, Vol 63, Pp 568-572 (2017)
Externí odkaz:
https://doaj.org/article/97650bc5130f49f29bbe8f6001638344
Paleoclimate proxy records from the North Atlantic region reveal substantially greater multi-centennial temperature variability during the Last Glacial Maximum (LGM) compared to the current interglacial. As there was no obvious change in external for
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6df1a27b37b5edd32a242c9ebb600935
https://doi.org/10.5194/egusphere-egu23-13276
https://doi.org/10.5194/egusphere-egu23-13276
According to geological records, the sea level during the Last Interglacial (∼ 129–116 ka) peaked 6 to 9 m higher than during the pre-industrial with a major contribution from the Antarctic ice sheet (Dutton et al. 2015). According to Clark et al
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2a440e2400572662ca57c184a673315e
https://doi.org/10.5194/egusphere-egu23-11678
https://doi.org/10.5194/egusphere-egu23-11678
Autor:
Paolo Scussolini, Job Dullaart, Sanne Muis, Alessio Rovere, Pepijn Bakker, Dim Coumou, Hans Renssen, Philip J. Ward, Jeroen C. J. H. Aerts
Publikováno v:
Climate of the Past, 19(1). European Geosciences Union
Scussolini, P, Dullaart, J C M, Muis, S, Rovere, A, Bakker, P, Coumou, D, Renssen, H, Ward, P & Aerts, J 2023, ' Modeled storm surge changes in a warmer world : the Last Interglacial ', Climate of the Past, vol. 19, no. 1, pp. 141–157 . https://doi.org/10.5194/cp-19-141-2023
Scussolini, P, Dullaart, J C M, Muis, S, Rovere, A, Bakker, P, Coumou, D, Renssen, H, Ward, P & Aerts, J 2023, ' Modeled storm surge changes in a warmer world : the Last Interglacial ', Climate of the Past, vol. 19, no. 1, pp. 141–157 . https://doi.org/10.5194/cp-19-141-2023
The Last Interglacial (LIG; ca. 125 ka) is a period of interest for climate research as it is the most recent period of the Earth's history when the boreal climate was warmer than at present. Previous research, based on models and geological evidence
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::53ba533361ffe1637fb8e1425d61b87f
https://research.vu.nl/en/publications/a3f21386-0329-4a57-b95e-40d980b83b19
https://research.vu.nl/en/publications/a3f21386-0329-4a57-b95e-40d980b83b19
Publikováno v:
Climate of the Past
Climate of the Past, 2022, 18 (11), pp.2523-2544. ⟨10.5194/cp-18-2523-2022⟩
Bakker, P, Goosse, H & Roche, D M 2022, ' Internal climate variability and spatial temperature correlations during the past 2000 years ', Climate of the Past, vol. 18, no. 11, pp. 2523-2544 . https://doi.org/10.5194/cp-18-2523-2022
Climate of the Past, 18(11), 2523-2544. European Geosciences Union
Climate of the Past, Vol. 18, no.11, p. 2523-2544 (2022)
eISSN
Climate of the Past, 2022, 18 (11), pp.2523-2544. ⟨10.5194/cp-18-2523-2022⟩
Bakker, P, Goosse, H & Roche, D M 2022, ' Internal climate variability and spatial temperature correlations during the past 2000 years ', Climate of the Past, vol. 18, no. 11, pp. 2523-2544 . https://doi.org/10.5194/cp-18-2523-2022
Climate of the Past, 18(11), 2523-2544. European Geosciences Union
Climate of the Past, Vol. 18, no.11, p. 2523-2544 (2022)
eISSN
The spatio-temporal structure of natural climate variability has to be taken into account when unraveling observed climatic changes and simulate future climate change. However, based on the comparison of temperature reconstructions and climate model
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6a945a85252a5c094c87b7fb2e363ebb
https://hal.science/hal-03917174/document
https://hal.science/hal-03917174/document
Autor:
Paolo Scussolini, Job Dullaart, Sanne Muis, Alessio Rovere, Pepijn Bakker, Dim Coumou, Hans Renssen, Philip J. Ward, Jeroen C. J. H. Aerts
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::543626788a244b95958a97c7baa0150d
https://doi.org/10.5194/egusphere-2022-101-supplement
https://doi.org/10.5194/egusphere-2022-101-supplement
The response of ice sheets to climate changes can be diverse and complex. The amplitude, speed and irreversibility of the melting of the ice sheets due to current anthropogenic emissions remain largely uncertain after 2100. Being able to reconstruct
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3f840f6ed38f6d92a401e09951f23c44
https://doi.org/10.5194/egusphere-egu22-5016
https://doi.org/10.5194/egusphere-egu22-5016