Zobrazeno 1 - 10
of 226
pro vyhledávání: '"H. Renssen"'
Autor:
E. Cruz-Silva, S. P. Harrison, I. C. Prentice, E. Marinova, P. J. Bartlein, H. Renssen, Y. Zhang
Publikováno v:
Climate of the Past, Vol 19, Pp 2093-2108 (2023)
There has been considerable debate about the degree to which climate has driven societal changes in the eastern Mediterranean region, partly through reliance on a limited number of qualitative records of climate changes and partly reflecting the need
Externí odkaz:
https://doaj.org/article/ba74af0f787045bcb845cdf5e6391c1a
Autor:
P. Scussolini, J. Dullaart, S. Muis, A. Rovere, P. Bakker, D. Coumou, H. Renssen, P. J. Ward, J. C. J. H. Aerts
Publikováno v:
Climate of the Past, Vol 19, Pp 141-157 (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://doaj.org/article/7ba19c8c92684929a2ca124af7a5872a
Publikováno v:
Climate of the Past, Vol 19, Pp 87-106 (2023)
This study presents the application of an interactive downscaling in Europe using iLOVECLIM (a model of intermediate complexity), increasing its atmospheric resolution from 5.56 to 0.25∘ kilometric. A transient simulation using the appropriate clim
Externí odkaz:
https://doaj.org/article/2d0e94c659b74084aba2bfaf41507a83
Publikováno v:
Climate of the Past, Vol 18, Pp 2303-2319 (2022)
The desertification and vegetation feedbacks of the “green Sahara” during the last interglacial (LIG) and the Holocene have been investigated by many studies. Yet the abruptness of climate and vegetation changes and their interactions are still u
Externí odkaz:
https://doaj.org/article/77c89779b81d46a6b0ed471f8a816b8a
Publikováno v:
Biogeosciences, Vol 18, Pp 1577-1599 (2021)
Lichen heaths are declining in abundance in alpine and Arctic areas partly due to an increasing competition with shrubs. This shift in vegetation types might have important consequences for the microclimate and climate on a larger scale. The aim of o
Externí odkaz:
https://doaj.org/article/1ff107b2b05a4e058002b3f0b92b5e8c
Autor:
M. Kageyama, S. Albani, P. Braconnot, S. P. Harrison, P. O. Hopcroft, R. F. Ivanovic, F. Lambert, O. Marti, W. R. Peltier, J.-Y. Peterschmitt, D. M. Roche, L. Tarasov, X. Zhang, E. C. Brady, A. M. Haywood, A. N. LeGrande, D. J. Lunt, N. M. Mahowald, U. Mikolajewicz, K. H. Nisancioglu, B. L. Otto-Bliesner, H. Renssen, R. A. Tomas, Q. Zhang, A. Abe-Ouchi, P. J. Bartlein, J. Cao, Q. Li, G. Lohmann, R. Ohgaito, X. Shi, E. Volodin, K. Yoshida, W. Zheng
Publikováno v:
Geoscientific Model Development, Vol 10, Pp 4035-4055 (2017)
The Last Glacial Maximum (LGM, 21 000 years ago) is one of the suite of paleoclimate simulations included in the current phase of the Coupled Model Intercomparison Project (CMIP6). It is an interval when insolation was similar to the present, but
Externí odkaz:
https://doaj.org/article/c45ad6ca172645069deb7104e231ef6a
Autor:
B. L. Otto-Bliesner, P. Braconnot, S. P. Harrison, D. J. Lunt, A. Abe-Ouchi, S. Albani, P. J. Bartlein, E. Capron, A. E. Carlson, A. Dutton, H. Fischer, H. Goelzer, A. Govin, A. Haywood, F. Joos, A. N. LeGrande, W. H. Lipscomb, G. Lohmann, N. Mahowald, C. Nehrbass-Ahles, F. S. R. Pausata, J.-Y. Peterschmitt, S. J. Phipps, H. Renssen, Q. Zhang
Publikováno v:
Geoscientific Model Development, Vol 10, Pp 3979-4003 (2017)
Two interglacial epochs are included in the suite of Paleoclimate Modeling Intercomparison Project (PMIP4) simulations in the Coupled Model Intercomparison Project (CMIP6). The experimental protocols for simulations of the mid-Holocene (midHolocen
Externí odkaz:
https://doaj.org/article/46caaf90ebbc43dcaf33ecd423978598
Publikováno v:
Climate of the Past, Vol 12, Iss 5, Pp 1119-1135 (2016)
The early Holocene is marked by the final transition from the last deglaciation to the relatively warm Holocene. Proxy-based temperature reconstructions suggest a Northern Hemisphere warming, but also indicate important regional differences. Model st
Externí odkaz:
https://doaj.org/article/409509a23d304703b5a1dd0da2865368
Publikováno v:
Geoscientific Model Development, Vol 8, Iss 7, Pp 2139-2151 (2015)
Recent modelling studies have indicated that icebergs play an active role in the climate system as they interact with the ocean and the atmosphere. The icebergs' impact is due to their slowly released meltwater, which freshens and cools the ocean and
Externí odkaz:
https://doaj.org/article/87f52e0d74b548f9b9da2c66bd55781b
Publikováno v:
The Cryosphere, Vol 9, Iss 3, Pp 821-835 (2015)
Icebergs have a potential impact on climate since they release freshwater over a widespread area and cool the ocean due to the take-up of latent heat. Yet, so far, icebergs have never been modelled using an ice-sheet model coupled to a global climate
Externí odkaz:
https://doaj.org/article/d627733c84af45aa97b330af54fa024f