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Atmospheric response to Arctic sea ice decline: results from PAMIP experiments
2021
Zenodo
We analyze the Northern Hemisphere atmospheric response to Arctic sea ice decline in the CNRM-CM6 model (130km resolution, 91 vertical levels) using atmosphere-only experiments that follow the PAMIP protocol described in Smith et al. (2019). The high-top atmospheric component of CNRM-CM6 is forced by the same pattern of SST but different idealized patterns of sea ice that correspond to i) pre-industrial conditions (PI), ii) present day conditions (PD), and iii) future conditions (FUT)
doi:10.5281/zenodo.4531291
fatcat:lgmc26xcd5gufcjeenu7dcasye