Zobrazeno 1 - 10
of 642
pro vyhledávání: '"G. Feulner"'
Autor:
M. Drüke, W. Lucht, W. von Bloh, S. Petri, B. Sakschewski, A. Tobian, S. Loriani, S. Schaphoff, G. Feulner, K. Thonicke
Publikováno v:
Earth System Dynamics, Vol 15, Pp 467-483 (2024)
Human activities have had a significant impact on Earth's systems and processes, leading to a transition of Earth's state from the relatively stable Holocene epoch to the Anthropocene. The planetary boundary framework characterizes major risks of des
Externí odkaz:
https://doaj.org/article/99fb5380158a4b058b0e05adebb7c831
Publikováno v:
Climate of the Past, Vol 19, Pp 2203-2235 (2023)
The Cryogenian period (720–635 million years ago) in the Neoproterozoic era featured two phases of global or near-global ice cover termed “snowball Earth”. Climate models of all kinds indicate that the inception of these phases must have occurr
Externí odkaz:
https://doaj.org/article/5458acd922d24be4b8ea3686dfcb6be2
Akademický článek
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Publikováno v:
Earth System Dynamics, Vol 14, Pp 533-547 (2023)
The instability with respect to global glaciation is a fundamental property of the climate system caused by the positive ice-albedo feedback. The atmospheric concentration of carbon dioxide (CO2) at which this Snowball bifurcation occurs changes thro
Externí odkaz:
https://doaj.org/article/7026d1e2d7974faf81c27ac3827d9486
Autor:
W. Weber
Publikováno v:
Annalen Der Physik
In my reply I present a re-analysis of the data of the Smithsonian Astrophysical Observatory (SAO). For this, a new data reduction method is introduced, allowing a drastic lowering of data scatter, so that the time series of the reduced data clearly
Autor:
M. Drüke, W. von Bloh, S. Petri, B. Sakschewski, S. Schaphoff, M. Forkel, W. Huiskamp, G. Feulner, K. Thonicke
Publikováno v:
Geoscientific Model Development, Vol 14, Pp 4117-4141 (2021)
The terrestrial biosphere is exposed to land-use and climate change, which not only affects vegetation dynamics but also changes land–atmosphere feedbacks. Specifically, changes in land cover affect biophysical feedbacks of water and energy, thereb
Externí odkaz:
https://doaj.org/article/63949aad474a4ce2877d2d63e5c9c9ca
Publikováno v:
Geoscientific Model Development, Vol 14, Pp 3697-3714 (2021)
The past and future evolution of the Antarctic Ice Sheet is largely controlled by interactions between the ocean and floating ice shelves. To investigate these interactions, coupled ocean and ice sheet model configurations are required. Previous mode
Externí odkaz:
https://doaj.org/article/342c238232844f26bd0d3fb32d3adcca
Autor:
G. S. Soreghan, L. Beccaletto, K. C. Benison, S. Bourquin, G. Feulner, N. Hamamura, M. Hamilton, N. G. Heavens, L. Hinnov, A. Huttenlocker, C. Looy, L. S. Pfeifer, S. Pochat, M. Sardar Abadi, J. Zambito
Publikováno v:
Scientific Drilling, Vol 28, Pp 93-112 (2020)
Chamberlin and Salisbury's assessment of the Permian a century ago captured the essence of the period: it is an interval of extremes yet one sufficiently recent to have affected a biosphere with near-modern complexity. The events of the Permian – t
Externí odkaz:
https://doaj.org/article/186c72805c514689849b258de602f65e
Publikováno v:
Environmental Research Letters, Vol 16, Iss 3, p 038002 (2021)
In their comment on our paper (Caesar et al 2020 Environ. Res. Lett. 15 024003), Chen and Tung (hereafter C&T) argue that our analysis, showing that over the last decades Atlantic meridional overturning circulation (AMOC) strength and global mean sur
Externí odkaz:
https://doaj.org/article/9849b9719af64063b3377d924f3d2886
Publikováno v:
Environmental Research Letters, Vol 15, Iss 2, p 024003 (2020)
According to established understanding, deep-water formation in the North Atlantic and Southern Ocean keeps the deep ocean cold, counter-acting the downward mixing of heat from the warmer surface waters in the bulk of the world ocean. Therefore, peri
Externí odkaz:
https://doaj.org/article/11d29d5607194082878602813fdeb5e9