CLIMBER-2: a climate system model of intermediate complexity. Part II: model sensitivity

By V. Petoukhov, A. Ganopolski, V. Brovkin, M. Claussen, A. Eliseev, C. Kubatzki, Stefan Rahmstorf. 2001

248 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/d27b49310ec37048e93c6a85a23e9c285ce8ae3c

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. A. Ganopolski
2. R. Calov
3. M. Claussen
4. Stefan Rahmstorf
5. Anders Levermann
6. V. Petoukhov
7. Ralf Greve
8. M. Vellinga

In Global and Planetary Change

1. Richard S. J. Tol
2. P. Link
3. Anders Levermann
4. A. Ganopolski
5. M. Vellinga
6. T. Kleinen
7. A. Griesel
8. R. Wood

In Oceanography

1. A. Ganopolski
2. T. Kleinen
3. A. Griesel
4. Richard S. J. Tol
5. R. Wood
6. Hermann Held
7. Matthias Hofmann
8. Stefan Rahmstorf

Citations in the corpus

• Possible economic impacts of a shutdown of the thermohaline circulation: an application of FUND (2004, background): “The characteristics of this climate model of intermediate complexity are described in detail in Petoukhov et al. (2000) and Ganopolski et al. (2001).”
• Detection of climate system bifurcations by degenerate fingerprinting (2004, methodology): “Model and Forcing [4] We use the oceanic output of CLIMBER2 [Petoukhov et al., 2000; Ganopolski et al., 2001] which is a coupled climate model of intermediate complexity.”
• Transient simulation of the last glacial inception. Part I: glacial inception as a bifurcation in the climate system (2005, background): “Its sensitivity to various climatological forcings is discussed in Ganopolski et al. (2001) .”
• Lowering of glacial atmospheric CO2 in response to changes in oceanic circulation and marine biogeochemistry (2007, unknown): “model, an oceanic biogeochemistry model, and a phosphatelimited model for marine biota [Petoukhov et al., 2000; Ganopolski et al., 2001; Brovkin et al., 2002a].”
• Global Climatic Impacts of a Collapse of the Atlantic Thermohaline Circulation (2002, result): “In the CLIMBER2 model Northern Hemisphere cooling associated with a climate state without THC (Ganapolski et al., 2001) has a pattern and amplitude similar to that in Figure 3.”
• On the driving processes of the Atlantic meridional overturning circulation (2007, background): “In zonally averaged models [Schmittner and Weaver, 2001; Ganopolski et al., 2001] the hysteresis loop shrinks with increasing vertical diffusion.”
• Rapid changes of glacial climate simulated in a coupled climate model (2001, methodology): “Model and background climate We use the CLIMBER-2 coupled climate model of intermediate complexit”