Snow, Water, Ice, Permafrost in the Arctic (SWIPA) - 2017
This subsite contains information products and materials presenting the results of the 2017 Snow, Water, Ice and Permafrost in the Arctic (SWIPA) assessment coordinated by AMAP - updating the earlier (2011) SWIPA assessment
The materials posted on this site are freely-available for non-commercial uses, including press/media use, and production of educational and outreach materials, etc. You are kindly requested to acknowledge AMAP as the source of these materials. Anyone wishing to use these materials for commercial purposes should contact amap@amap.no.
All available PDF files are (c) Arctic Monitoring and Assessment Programme (AMAP) and are intended for individual viewing and personal use and should not be posted on other websites or otherwise distributed in electronic or print form.
Reports
The results of the SWIPA assessment are presented in reports, targetting different audiences. The results of the 2017 SWIPA assessment are currently available in a Summary for Policy-Makers and series of Fact Sheets. The detailed technical background that is the basis for the other reports will be availble in the summaer of 2017.
Videos
Short (ca. 3 minute) and Full length (ca. 15 minute) videos presenting the SWIPA assessment and its results.
All SWIPA videos (3 films in long and short versions, also in multiple languages) are available from the AMAP Vimeo channel
Time-lapse movie clips
Available for non-commercial uses, including press/media use, and production of educational and outreach materials, etc. Click the links to play/download. You are kindly requested to acknowledge the indicated sources of these movie clips.





Photographs
Selection of photographs available for non-commercial uses, including press/media use, and production of educational and outreach materials, etc. Click the photos for full-size versions. You are kindly requested to acknowledge the indicated sources of these photos.

Surface meltwater disappears down a moulin. Near the ice margin in the Ilulissat region, West Greenland. © Konrad Steffen/CIRES, University of Colorado

Clearing snow drifts in downtown areas is an almost constant job. NEEM ice coring camp at the Greenland Ice Sheet, 77°27’N / 51°04’W, 2454 m altitude. © NEEM ice core drilling project, www.neem.ku.dk

The international flag line in the main street of the
NEEM ice coring camp at the Greenland Ice Sheet, 77°27’N / 51°04’W, 2454 m altitude © NEEM ice core drilling project, www.neem.ku.dk

Scientists and drillers at work in the sub-surface drill trench. NEEM ice coring camp at the Greenland Ice Sheet, 77°27’N / 51°04’W, 2454 m altitude © NEEM ice core drilling project, www.neem.ku.dk

The long-term research platform, Swiss Camp, at ca. 1100 m above sea level on the Greenland Ice Sheet (69°30’N / 49°20’W) northeast of Ilulissat, West Greenland © Konrad Steffen/CIRES, Univ. of Colorado

Iceberg being discharged from the glacier front of Jakobshavn Isbræ. Near Ilulissat, West Greenland © Martin Truffer/University of Alaska-Fairbanks

Drained glacier dammed meltwater lake reveals walls of bue ice. Near Helheim Glacier, Southeast Greenland © Henrik Egede Lassen/Alpha Film

Soil particles on the ice sheet surface near the margins further accelerate the melting process © Henrik Egede Lassen/Alpha Film

Meltwater from the ice sheet surface is drained through a moulin. The edge zone in the Ilulissat region, West Greenland © Konrad Steffen/CIRES, University of Colorado

Scientist from Ohio State University awaiting pick-up after installing a GNET GPS station on Timmiariit Island, SE Greenland, as part of the research efforts to estimate ice mass changes in the Greenland Ice Sheet © Dana Caccamise, Ohio State University

Heavily crevassed area of Jakobshavn Isbræ near the glacier front. Ilulissat, West Greenland © Konrad Steffen/CIRES, University of Colorado




















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