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Showing 1–4 of 4 results
Advanced filters: Author: Edward Blanchard-Wrigglesworth Clear advanced filters

  • Summer snow accumulation and its albedo effect on Arctic sea ice are controlled by the Arctic Oscillation atmospheric circulation pattern, according to a combined modelling and remote sensing analysis.

    • Melinda A. Webster
    • Aku Riihelä
    • Linette Boisvert
    ResearchOpen Access
    Nature Geoscience
    Volume: 17, P: 995-1002

  • The atmospheric circulation during the sea-ice maximum significantly impacts year-round Antarctic sea-ice area, with recent circulation changes having a notable, and previously overlooked, signature in recent ice losses, according to observational analysis.

    • Chloe L. Boehm
    • David W. J. Thompson
    • Edward Blanchard-Wrigglesworth
    ResearchOpen Access
    Communications Earth & Environment
    Volume: 6, P: 1-11

  • 70% of the Antarctic sea ice area’s record low anomaly in 2023 was due to warm Southern Ocean sea surface temperatures, while 30% was due to atmospheric circulation, and the transition from La Niña to El Niño had minimal impact, according to results from a fully-coupled Earth system model nudged to observed atmospheric circulation.

    • Zachary I. Espinosa
    • Edward Blanchard-Wrigglesworth
    • Cecilia M. Bitz
    ResearchOpen Access
    Communications Earth & Environment
    Volume: 5, P: 1-9

  • Projections of Arctic sea-ice loss vary significantly between global circulation models. Analysis of the CMIP5 ensemble reveals that these differences can be related to background ice thickness and corresponding growth/melt processes, and not variations in the sea-ice model used.

    • François Massonnet
    • Martin Vancoppenolle
    • Edward Blanchard-Wrigglesworth
    Research
    Nature Climate Change
    Volume: 8, P: 599-603