Abigail Ahlert and Clara Burgard The scientific questions that will be studied * Why do climate models in CMIP3 and CMIP5 have limited skill in reproducing the sea ice relationships…
Ed Blockley (ed.blockley[@]metoffice.gov.uk), Met Office Hadley Centre Arctic summer sea ice cover has declined at a rate of 13% per decade since satellite observation began, and there is much interest…
Lead: Axel Schweiger (axel[@]apl.uw.edu)Current Sea Ice Reanalyses offer time and space complete representations of sea ice parameters for the satellite period (1979-present). In order to obtain a better understanding of…
The Presentation given by Dr. Regine Hock, GlacierMIP Co-Chair, at the WCRP-CLIVAR/IOC-UNESCO Regional Sea Level Changes and Coastal Impacts Conference, July 10-14 2017, Columbia University New York (USA) is availale.…
--GlacierMIP is a CliC sponsored activity The Minutes of the GlacierMIP meeting held on February 17, 2017, in conjunciton with the IGS/IACS/CliC International Symposium on the Cryosphere in a Changing…
Daniel Senftleben (daniel.senftleben[@]dlr.de) and Nikolay Koldunov (nikolay.koldunov[@]awi.de)The issue:Interpolating gridded data from one spatial grid to another (from here on termed “regridding”) is necessary when two datasets on different grids are to…
The June 2017 Update on the Permafrost Carbon Network latest activities is available at: http://arcticportal.org/ap-library/news/1915-activities-of-the-permafrost-carbon-network
Alek Petty (alek.a.petty[@]nasa.gov)The scientific questions that will be studied:This theme will investigate snow on sea ice in CMIP6 models. As our knowledge of snow on sea ice in global climate…
The June 2017 CliC Newsletter No. 26 is available online. It includes three science features: one on recent changes to New Zealand glaciers, another looks at phytoplankton blooms observed under…
François Massonnet (francois.massonnet[@]uclouvain.be) and Martin Vancoppenolle (martin.vancoppenolle[@]locean-ipsl.upmc.fr). The scientific questions that will be studied:-What is the importance of local and/or non-radiative feedbacks in which sea ice is involved, for sea ice…