Zobrazeno 1 - 10
of 20
pro vyhledávání: '"Claudia Kubatzki"'
Publikováno v:
Global Ecology and Biogeography. 19:278-286
Aim Atmospheric CO2 concentrations depend, in part, on the amount of biomass locked up in terrestrial vegetation. Information on the causes of a broad-scale vegetation transition and associated loss of biomass is thus of critical interest for underst
Autor:
Eva Alram-Stern, Gary O. Rollefson, Eva Bauer, Bernhard Weninger, Olaf Jöris, Claudia Kubatzki, Tjeerd H. van Andel, Uwe Danzeglocke, Lee Clare, Henrieta Todorova
Publikováno v:
Quaternary Research. 66:401-420
We explore the hypothesis that the abrupt drainage of Laurentide lakes and associated rapid switch of the North Atlantic thermohaline circulation 8200 yr ago had a catastrophic influence on Neolithic civilisation in large parts of southeastern Europe
Publikováno v:
Climate Dynamics. 27:333-344
We investigate the sensitivity of simulations of the last glacial inception (LGI) with respect to initial (size of the Greenland ice sheet) and surface (state of ocean/vegetation) conditions and two different CO2 reconstructions. Utilizing the CLIMBE
Publikováno v:
Climatic Change. 69:409-417
Recently, W.F. Ruddiman (2003, Climatic Change, Vol. 61, pp. 261–293) suggested that the anthropocene, the geological epoch of significant anthropospheric interference with the natural Earth system, has started much earlier than previously thought
Autor:
H. Becker Weg, Claudia Kubatzki, Andrey Ganopolski, Vladimir Petoukhov, Victor Brovkin, Martin Claussen
Publikováno v:
Climatic Change. 57:99-118
By using a climate system model of intermediate complexity, we have simulated long- term natural climate changes occurring over the last 9000 years. The paleo-simulations in which the model is driven by orbital forcing only, i.e., by changes in insol
Publikováno v:
EPIC3Climate dynamics, 16, pp. 799-814
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The climate at the Last Interglacial Maximum (125 000 years before present) is investigated with the atmosphere-ocean general circulation model ECHAM-1/LSG and with the climate system model of intermediate complexity CLIMBER-2. Comparison of the resu
Publikováno v:
Global Ecology and Biogeography. 8:509-517
climate with other forcings, climate responses to the changing atmospheric CO2 concentration and In order to estimate the eVect of historical land solar irradiance are also analysed. When all three cover change (deforestation) on climate, we perform
Autor:
Martin Claussen, Claudia Kubatzki, Andrey Ganopolski, Stefan Rahmstorf, Vladimir Petoukhov, Victor Brovkin
Publikováno v:
Environmental Modeling and Assessment. 4:209-216
We present a new reduced-form model for climate system analysis. This model, called CLIMBER-2 (for CLIMate and BiosphERe, level 2), fills the current gap between simple, highly parameterized climate models and computationally expensive coupled models
Publikováno v:
EPIC3Science, 280, pp. 1916-1919
Simulations with a synchronously coupled atmosphere–ocean–vegetation model show that changes in vegetation cover during the mid-Holocene, some 6000 years ago, modify and amplify the climate system response to an enhanced seasonal cycle of solar i
Autor:
Frank Sirocko, Martin Claussen, Thomas Litt, Maria Fernanda Sánchez Goñi, Andre Berger, Tatjana Boettger, Markus Diehl, Stéphanie Desprat, Barbara Delmonte, Detlev Degering, Manfred Frechen, Mebus A. Geyh, Matthias Groeger, Masa Kageyama, Frank Kaspar, Norbert Kühl, Claudia Kubatzki, Gerrit Lohmann, Marie-France Loutre, Ulrich Müller, Bert Rein, Wilfried Rosendahl, Katy Roucoux, Denis-Didier Rousseau, Klemens Seelos, Mark Siddall, Denis Scholz, Christoph Spötl, Brigitte Urban, Maryline Vautravers, Andrei Velichko, Stefan Wenzel, Martin Widmann, Bernd Wünnemann
Publisher Summary The last four interglacials (intervals during which global ice volume was similar to, or less than, that of our current warm stage) correspond to the warmest parts of the marine oxygen isotope stages marine isotopic age (MIS) 5, 7,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::47e92126761ed806a33d68d4a9fa115a
https://doi.org/10.1016/s1571-0866(07)80065-0
https://doi.org/10.1016/s1571-0866(07)80065-0