Role of the ice sheets in the climatic system: Interactions analysis between an Antarctic ice sheet model and a climate model

• Main Author: Philippon, Gwenaëlle
• Other Authors: Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA), Université Pierre et Marie Curie - Paris VI, Gilles Ramstein([e-mail])
• Format: Doctoral or Postdoctoral Thesis
• Language: French
• Published: HAL CCSD 2007
• Subjects: Antarctic; Feedbacks; climatic model; ice sheet model; paleoclimate; last deglaciation; Climate; ice sheet Interactions; Interactions climat; calotte de glace; Antarctique; Rétroactions; modè le de climat; modèle de calotte de glace; paléoclimat; dernière déglaciation; [SDU.STU]Sciences of the Universe [physics]/Earth Sciences; The Antarctic; South Pole; Antarc*; Antarctique*; Ice Sheet; North Atlantic; South pole
• Online Access: https://theses.hal.science/tel-00328184; https://theses.hal.science/tel-00328184/document; https://theses.hal.science/tel-00328184/file/ThesePhilippon_poidsplume.pdf.pdf

The climatic system includes several components with different characteristic time scales (i.e. the atmosphere, the hydrosphere, the biosphere, the lithosphere and the cryosphere). The Antarctic ice-sheet represents the main contribution of the latter component. The south pole continent contains 70% of the fresh water supply of the Earth and 91% of the ice on Earth. If all the ice were melt, it would lead to a sea level rise of about 60 m. Within the content of global warming of the Earth, the polar regions are very sensitive. Observations by satellites show that the Antarctic continent is subjected to abrupt temperature changes which are likely to be induced by atmospheric greenhouse gases. This implies large ice collapses and a great acceleration of the ice flow, which then goes to the ocean. To better study the evolution of future climate, one can look in the past whether such collapses ever happened. The aim of this work is to study the interactions between climate and ice sheets, especially the Antarctic ice sheet. I have developed a coupling method between an Antarctic ice sheet model and a climate model of intermediate complexity, which was first coupled with a northern hemisphere ice sheet model. In the first part, I have tested this new tool to understand processes occurring during the last major collapse of northern and southern ice sheets (i.e. the last deglaciation, 21 kyr BP). In the second part, I have tried to evaluate the present and past climate sensitivities to external freshwater discharges delivered in sensitive areas of both the North Atlantic and the Southern oceans. The ice sheets seem sensitive to the climate forcing (insolation and CO2) and respond also to the climatic variability induced by ice melting itself. The Quaternary period is one of the rare period in the Earth history where such ice sheets were present. Studying the interactions of these ice sheets with the climate is therefore an important challenge, both for past and future climate investigations. Le système climatique fait ...