2017/01/05 by Wei Liu, Shang‐Ping Xie, Zhengyu Liu +1 · 11 citations
Earth and Planetary Sciences · Environmental Science · #Geology and Paleoclimatology Research #Climate variability and models #Oceanographic and Atmospheric Processes
paper · pdf · doi:10.1126/sciadv.1601666
openalex publication_date 2017/01/05 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/31
concentration is abruptly doubled from the 1990 level. Compared to an uncorrected model, the AMOC collapse brings about large, markedly different climate responses: a prominent cooling over the northern North Atlantic and neighboring areas, sea ice increases over the Greenland-Iceland-Norwegian seas and to the south of Greenland, and a significant southward rain-belt migration over the tropical Atlantic. Our results highlight the need to develop dynamical metrics to constrain models and the importance of reducing model biases in long-term climate projection.