Importance of physics, resolution and forcing in hindcast simulations of Arctic and Antarctic sea ice variability and trends
By François Massonnet, T. Fichefet, Hugues Goosse, M. Vancoppenolle, C. K. Beatty, P. Mathiot. 2010
700 citations recorded by the source corpus.
View Paper: https://www.semanticscholar.org/paper/7f48289cafe60ecb7d451475b658027b626c2628
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Citations in the corpus
- What caused Earths temperature variations during the last 800,000 years? Data-based evidences on radiative forcing and constraints on climate sensitivity (2009, background): “The glacial increase in annual mean sea ice area between present (Cavalieri and Parkinson, 2008; Parkinson and Cavalieri, 2008) and the LGM (CLIMAP, 1976; Sarnthein et al.”
- At the rainbow’s end: high productivity fueled by winter upwelling along an Arctic shelf (2014, background): “…is also characterized by large interannual and decal variability with respect to sea-ice extent (Vinje 1999) and the overall decline in both sea-ice concentration and sea-ice extent in the Arctic since 1979 are widely documented (e.g., Parkinson and Cavalieri 2008; Comiso et al. 2008; Comiso 2012).”
- On the formulation of sea-ice models. Part 1: Effects of different solver implementations and parameterizations (2010, background): “For example, Dey (1981) estimates an inflow into Baffin Bay of 504 370 to 537 km(3) yr−1 but a flow of only 102 to 137 km(3) yr−1 further upstream in 505 Barrow Strait in the 1970’s from satellite images; Aagaard and Carmack (1989) 506 give approximately 155 km(3) yr−1 for the export through the CAA”
- Climate change and the increasing impact of polar bears on bird populations (2015, background): “The large spatial variation in sea ice abundance and rate of disappearance over the years corresponds to patterns found at the scale of the entire Arctic (Cavalieri and Parkinson, 2012; Meier et al., 2014).”
- Parameterizing the fresh-water flux from land ice to ocean with interactive icebergs in a coupled climate model (2010, background): “With 15.3 106 km2 the model’s sea-ice extent exceeds the observed long-term (1979–2006) average of 11.5 106 km2 (Cavalieri and Parkinson, 2008) by one-third.”