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  1. Article

    Open Access

    Response of the Greenland and Antarctic Ice Sheets to Multi-Millennial Greenhouse Warming in the Earth System Model of Intermediate Complexity LOVECLIM

    Calculations were performed with the Earth system model of intermediate complexity LOVECLIM to study the response of the Greenland and Antarctic ice sheets to sustained multi-millennial greenhouse warming. Use...

    P. Huybrechts, H. Goelzer, I. Janssens, E. Driesschaert in Surveys in Geophysics (2011)

  2. No Access

    Article

    Impact of Greenland and Antarctic ice sheet interactions on climate sensitivity

    We use the Earth system model of intermediate complexity LOVECLIM to show the effect of coupling interactive ice sheets on the climate sensitivity of the model on a millennial time scale. We compare the respon...

    H. Goelzer, P. Huybrechts, M. F. Loutre, H. Goosse, T. Fichefet in Climate Dynamics (2011)

  3. No Access

    Article

    Key features of the IPSL ocean atmosphere model and its sensitivity to atmospheric resolution

    This paper presents the major characteristics of the Institut Pierre Simon Laplace (IPSL) coupled ocean–atmosphere general circulation model. The model components and the coupling methodology are described, as...

    Olivier Marti, P. Braconnot, J.-L. Dufresne, J. Bellier, R. Benshila in Climate Dynamics (2010)

  4. No Access

    Article

    Impact of transient freshwater releases in the Southern Ocean on the AMOC and climate

    The bipolar ocean seesaw is a process that explains the competition between deep waters formed in the North Atlantic (NA) and in the Southern Ocean (SO). In this picture, an increase in the rate of formation o...

    Didier Swingedouw, T. Fichefet, H. Goosse, M. F. Loutre in Climate Dynamics (2009)

  5. No Access

    Article

    The spatial and temporal complexity of the Holocene thermal maximum

    The period of relatively warm climate from 11,000 to 5,000 years ago was marked by considerable temporal and spatial variability. Model simulations relate this complexity to the influence of the waning Laurent...

    H. Renssen, H. Seppä, O. Heiri, D. M. Roche, H. Goosse, T. Fichefet in Nature Geoscience (2009)

  6. No Access

    Article

    Analysis of the projected regional sea-ice changes in the Southern Ocean during the twenty-first century

    Using the set of simulations performed with atmosphere-ocean general circulation models (AOGCMs) for the Fourth Assessment Report of the Intergovernmental Panel on Climate Change (IPCC AR4), the projected regi...

    W. Lefebvre, H. Goosse in Climate Dynamics (2008)

  7. No Access

    Chapter

    Regional Response of the Climate System to Solar Forcing: The Role of the Ocean

    A coupled climate model is used to explore the regional response of the climate system to solar forcing, with emphasis on the role of the ocean. It is shown that both the transient and the equilibrium response...

    H. Goosse, H. Renssen in Solar Variability and Planetary Climates (2007)

  8. No Access

    Article

    Evaluation of different freshwater forcing scenarios for the 8.2 ka BP event in a coupled climate model

    To improve our understanding of the mechanism causing the 8.2 ka BP event, we investigated the response of ocean circulation in the ECBilt-CLIO-VECODE (Version 3) model to various freshwater fluxes into the La...

    A. P. Wiersma, H. Renssen, H. Goosse, T. Fichefet in Climate Dynamics (2006)

  9. No Access

    Article

    Regional Response of the Climate System to Solar Forcing: The Role of the Ocean

    A coupled climate model is used to explore the regional response of the climate system to solar forcing, with emphasis on the role of the ocean. It is shown that both the transient and the equilibrium response...

    H. Goosse, H. Renssen in Space Science Reviews (2006)

  10. No Access

    Article

    EMIC Intercomparison Project (EMIP–CO2): comparative analysis of EMIC simulations of climate, and of equilibrium and transient responses to atmospheric CO2 doubling

    An intercomparison of eight EMICs (Earth system Models of Intermediate Complexity) is carried out to investigate the variation and scatter in the results of simulating (1) the climate characteristics at the pr...

    V. Petoukhov, M. Claussen, A. Berger, M. Crucifix, M. Eby in Climate Dynamics (2005)

  11. No Access

    Article

    Changes in European precipitation seasonality and in drought frequencies revealed by a four-century-long tree-ring isotopic record from Brittany, western France

    A new paleoclimatic reconstruction for western France is obtained from tree-ring cellulose stable isotopes. Living trees from Rennes Forest and beams from two ancient buildings in Rennes city have been combine...

    V. Masson-Delmotte, G. Raffalli-Delerce, P. A. Danis, P. Yiou in Climate Dynamics (2005)

  12. No Access

    Article

    Surface temperature control in the North and tropical Pacific during the last glacial maximum

    Based on coupled modelling evidence we argue that topographically-induced modifications of the large-scale atmospheric circulation during the last glacial maximum may have led to a reduction of the westerlies...

    A. Timmermann, F. Justino, F.-F **, U. Krebs, H. Goosse in Climate Dynamics (2004)

  13. No Access

    Article

    Exciting natural modes of variability by solar and volcanic forcing: idealized and realistic experiments

    Using multi-millenium simulations performed with the three-dimensional climate model ECBILT-CLIO, we analyze how variations in the external forcing can excite low-frequency modes of climate variability. We fi...

    H. Goosse, H. Renssen in Climate Dynamics (2004)

  14. No Access

    Article

    Large sea-ice volume anomalies simulated in a coupled climate model

    The processes leading to the formation of a large anomaly of sea-ice volume integrated over the Northern Hemisphere have been investigated in a coarse-resolution three-dimensional atmosphere–ocean-sea-ice mode...

    H. Goosse, F. Selten, R. Haarsma, J. Opsteegh in Climate Dynamics (2003)

  15. No Access

    Article

    A mechanism of decadal variability of the sea-ice volume in the Northern Hemisphere

    A long-term simulation performed with a coarse-resolution, global, atmosphere–ocean–sea-ice model displays strong decadal variability of the sea-ice volume in the Northern Hemisphere with a significant peak at...

    H. Goosse, F. Selten, R. Haarsma, J. Opsteegh in Climate Dynamics (2002)

  16. No Access

    Article

    Earth system models of intermediate complexity: closing the gap in the spectrum of climate system models

    We propose a new perspective on the hierarchy of climate models which goes beyond the "classical" climate modeling pyramid that is restricted mainly to atmospheric processes. Most notably, we introduce a new ...

    M. Claussen, L. Mysak, A. Weaver, M. Crucifix, T. Fichefet in Climate Dynamics (2002)

  17. No Access

    Chapter and Conference Paper

    The “hidden torque”: the art, for a torque, to dominate everywhere and appear in no equation

    The effect of the superficial fluid layers (atmosphere and ocean) on the Earth rotation occurs by means of three torques: the pressure torque (or mountain torque) arising from a difference of pressure on the t...

    O. de Viron, V. Dehant, H. Goosse in Vistas for Geodesy in the New Millennium (2002)

  18. No Access

    Chapter

    A Modelling Approach to the Ross Sea Plankton Ecosystem

    A conceptual and numerical model adapted to the local plankton ecosystem (ECOHYDROMVG) has been developed on the basis of the information acquired during various oceanographic cruises in the Ross Sea. The cons...

    J. H. Hecq, L. Guglielmo, A. Goffart, G. Catalano, H. Goosse in Ross Sea Ecology (2000)

  19. No Access

    Article

    Sensitivity of a global ice–ocean model to the Bering Strait throughflow

     To understand the influence of the Bering Strait on the World Ocean’s circulation, a model sensitivity analysis is conducted. The numerical experiments are carried out with a global, coupled ice–ocean model. ...

    H. Goosse, J. M. Campin, T. Fichefet, E. Deleersnijder in Climate Dynamics (1997)