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teleconnections and of changing spatial heterogeneities in both the AMOC and the Amazon. In the specific sub-project at IMAU, existing GCM simulations in which AMOC undergoes a collapse will be analysed
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densification model forced by high resolution output from the regional climate model RACMO to simulate the evolution of the Larsen C firn layer in the recent past (1950 to present) and into the future (up to 2100
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