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Programme for Monitoring of the Greenland Ice Sheet (PROMICE)Quantifying the mass loss of the Greenland ice sheet
http://www.promice.org/
Quantifying the mass loss of the Greenland ice sheet
http://www.promice.org/
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Programme for Monitoring of the Greenland Ice Sheet (PROMICE) | promice.org Reviews
https://promice.org
Quantifying the mass loss of the Greenland ice sheet
promice.org
Programme for Monitoring of the Greenland Ice Sheet (PROMICE)
http://www.promice.org/home.html;jsessionid=9BF9CE1B55E8A3DB1AC456F69CE9AD31
Historical Mass Balance Data. Greenland is the world's largest island, larger than France, Germany, the UK, Spain and Italy combined. Greenland is host to the second largest ice mass on the planet, covering 82% of the island. Area of all ice in Greenland: 1.8×10. Volume of the ice sheet: 3.0×10. Mass of the ice sheet: 2.7×10. Maximum ice sheet elevation: 3275 m. Maximum ice sheet thickness: 3367 m. Lowest elevation of the ice sheet bed: -555 m. Age of the ice sheet: 2.4 million years.
Programme for Monitoring of the Greenland Ice Sheet (PROMICE)
http://www.promice.org/GletsjerkortDownload.html;jsessionid=9BF9CE1B55E8A3DB1AC456F69CE9AD31
Historical Mass Balance Data. Download Greenland ice cover. A PROMICE grid of fractional ice cover with 1 km postings and 5 km postings are available for everyone and at no charge. If interested in using the data, please make a request by filling in the form. Also, please include a few sentences stating how you intend to use the data. The grids were produced from the vectors map by Citterio and Ahlstrøm (2013). To exactly match the projection and extent of the datasets by Bamber et al. (2013).
Programme for Monitoring of the Greenland Ice Sheet (PROMICE)
http://www.promice.org/FlowingIce.html;jsessionid=9BF9CE1B55E8A3DB1AC456F69CE9AD31
Historical Mass Balance Data. Ice flows from the high interior to the margin of the Greenland ice sheet where it either melts or is lost to iceberg calving. Ice flows faster in a warmer climate, because meltwater originating from the surface reduces friction at the bottom of the ice sheet. Increased iceberg calving from outlet glaciers, often termed the ice-dynamic mass loss, is responsible for a substantial part of the mass loss of the Greenland ice sheet. Timelapse of calving glacier in Greenland.
Programme for Monitoring of the Greenland Ice Sheet (PROMICE)
http://www.promice.org/Isskolen.html;jsessionid=9BF9CE1B55E8A3DB1AC456F69CE9AD31
Historical Mass Balance Data. PROMICE was launched by The Danish. Energy Agency DANCEA programme to. Assess changes in the Greenland ice sheet. Contact PROMICE: info@promice.dk. PROMICE is operated by GEUS. In collaboration with DTU Space. Geological Survey of Denmark and Greenland (GEUS).
Programme for Monitoring of the Greenland Ice Sheet (PROMICE)
http://www.promice.org/promicePublications.html;jsessionid=9BF9CE1B55E8A3DB1AC456F69CE9AD31
Historical Mass Balance Data. Andresen CS, Hansen MJ, Seidenkrantz M-S, Jennings AE, Knudsen MF, Nørgaard-Pedersen N, Larsen NK, Kuijpers A and Pearce C (2013) Mid- to late-Holocene oceanographic variability on the Southeast Greenland shelve. Holocene, 23 (2), 167-178 (doi: 10.1177/0959683612460789). Citterio M and Ahlstrøm AP (2013) Brief communication "The aerophotogrammetric map of Greenland ice masses". Cryosph., 7, 445-449 (doi: 10.5194/tc-7-445-2013). Machguth H, Rastner P, Bolch T, Mölg N, Sa...
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News - Professor Jason E. Box
http://jasonbox.net/news
Follow Jason Box Twitter. North Pole Overheating 2016. Climate Change Communication Residency, Oregon July 3-14 , 2017. Don’t Mess With Me, I’m a Scientist. Separation of Manhattan Is. sized ice shelf pieces from 79 Glacier far northeastern Greenland. More Greenland melt under cloudy conditions. Dr Jason E. Box. Professor Jason E. Box. North Pole Overheating 2016. December 25, 2016. The combination of 1.) extra ocean to atmosphere heat transfer enabled by record low sea ice. The patterns in the two time ...
more Greenland melt under cloudy conditions - Professor Jason E. Box
http://jasonbox.net/more-greenland-melt-under-cloudy-conditions
Follow Jason Box Twitter. North Pole Overheating 2016. Climate Change Communication Residency, Oregon July 3-14 , 2017. Don’t Mess With Me, I’m a Scientist. Separation of Manhattan Is. sized ice shelf pieces from 79 Glacier far northeastern Greenland. More Greenland melt under cloudy conditions. Dr Jason E. Box. Professor Jason E. Box. More Greenland melt under cloudy conditions. April 1, 2016. On the late December 2015 northern temperature anomalies. More than under sunny conditions. A persistent air fl...
About the August, 2014 dark Greenland photos - Dark Snow Project
http://darksnow.org/about-the-august-2014-dark-greenland-photos
Like Us On Facebook. Follow Us On Twitter. Dark Snow is a crowd funded activity. May 11, 2016. Black and Bloom: Sheffield Update. May 1, 2016. Sculptural products from Dark Snow 2014 campaign. April 28, 2016. Greenland ice albedo decline. October 22, 2015. Record setting 2015 North American fire radiative power – 2.5x the 2000-2015 average. July 25, 2015. About the August, 2014 dark Greenland photos. October 29, 2014. Climate stations and an extreme ice survey. Time lapse camera went viral,. Benning, L&#...
Dark Snow Project - Page 2 of 8 -
http://darksnow.org/page/2
Like Us On Facebook. Follow Us On Twitter. Dark Snow is a crowd funded activity. May 11, 2016. Black and Bloom: Sheffield Update. May 1, 2016. Sculptural products from Dark Snow 2014 campaign. April 28, 2016. Greenland ice albedo decline. October 22, 2015. Record setting 2015 North American fire radiative power – 2.5x the 2000-2015 average. July 25, 2015. We believe gathering measurements from the surface of Greenland ice is fundamental to advancing our understanding of the melting Arctic. May 29, 2015.
Mining for (data) gold – Sterna Paradisaea
https://sternaparadisaea.net/2015/05/29/mining-for-data-gold
Arctic, climate, science, nature. Climate change at the local scale. A Sea-Ice Free Arctic in 2016? How pristine is the Arctic? Bless the rains down in Africa #DACEA3. Ben Goldacre's Bad Science blog. Bird of the sun. High Heels in the Lab. Enter your email address to follow this blog and receive notifications of new posts by email. Join 13 other followers. Mining for (data) gold. Comparison with Promice KPC U station observations and HIRHAM5 modelled monthly mean temperatures. And the Climate Lab Boo.
May 2015 – Sterna Paradisaea
https://sternaparadisaea.net/2015/05
Arctic, climate, science, nature. Climate change at the local scale. A Sea-Ice Free Arctic in 2016? How pristine is the Arctic? Bless the rains down in Africa #DACEA3. Ben Goldacre's Bad Science blog. Bird of the sun. High Heels in the Lab. Enter your email address to follow this blog and receive notifications of new posts by email. Join 13 other followers. Mining for (data) gold. Comparison with Promice KPC U station observations and HIRHAM5 modelled monthly mean temperatures. And the Climate Lab Boo.
Meltfactor » 2013 » September
http://meltfactor.org/2013/09
The ice and climate blog of Jason Box, PhD. Archive for September, 2013. Phoenix Glacier relic ice. Tuesday, September 10th, 2013. I’m in South Greenland drilling low tech metal pipes into the ice to calibrate high tech satellite, aircraft, and model data. Flying over this landscape, it’s stunning how much the ice has retreated. I was stunned to witness (and photograph) more stranded relic ice on the sides of the glacier. Notice how no ice is feeding Phoenix’s wings from upstream. This Phoenix should of ...
Meltfactor » 2013 » August
http://meltfactor.org/2013/08
The ice and climate blog of Jason Box, PhD. Archive for August, 2013. Visiting and monitoring South Greenland dark ice. Friday, August 16th, 2013. I’m spending a week flying out of Narsarsuaq, south Greenland, with colleague Dr. Robert Fausto, to maintain climate stations equipped to monitor surface ice melt in great detail. Part of the Danish PROMICE network. The stations obtain surface energy and mass budget closure. The closure means that calculated melt matches with observed melt. Photo J. Box. Rober...
Glacier Bytes
http://williamcolgan.net/blog
Suppressed Melt Percolation in Greenland Firn. Posted by William Colgan. On May 19, 2016. We have a new open-access study in the current volume of Annals of Glaciology. That tracks the fate of meltwater in the relatively porous near-surface firn of the Greenland Ice Sheet using temperature sensors. Figure 1 – Lead author Charalampos Charalampidis drilling a borehole on the Greenland Ice Sheet near KAN U during the 2013 spring field campaign. Figure 2 – Automated observations of firn temperatures in...
Om Polar Portal: Polar Portal
http://polarportal.dk/om-polar-portal
Velkommen til Polar Portal. Her formidler DMI, GEUS og DTU Space de seneste observationer og den nyeste viden om is- og klimaudviklingen i Arktis. På polarportal.dk stiller danske forskningsinstitutioner deres viden om havisen i Arktis og den grønlandske indlandsis til rådighed for den danske og internationale offentlighed. Portalens hovedformål er at gøre det muligt for offentligheden at få indblik i den overvågning af isen, som foretages. Har ligeledes reageret markant på temperaturstigningerne. Ov...
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Programme for Monitoring of the Greenland Ice Sheet (PROMICE)
Historical Mass Balance Data. Greenland is the world's largest island, larger than France, Germany, the UK, Spain and Italy combined. Greenland is host to the second largest ice mass on the planet, covering 82% of the island. Area of all ice in Greenland: 1.8×10. Volume of the ice sheet: 3.0×10. Mass of the ice sheet: 2.7×10. Maximum ice sheet elevation: 3275 m. Maximum ice sheet thickness: 3367 m. Lowest elevation of the ice sheet bed: -555 m. Age of the ice sheet: 2.4 million years.
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Programme for Monitoring of the Greenland Ice Sheet (PROMICE)
Historical Mass Balance Data. Greenland is the world's largest island, larger than France, Germany, the UK, Spain and Italy combined. Greenland is host to the second largest ice mass on the planet, covering 82% of the island. Area of all ice in Greenland: 1.8×10. Volume of the ice sheet: 3.0×10. Mass of the ice sheet: 2.7×10. Maximum ice sheet elevation: 3275 m. Maximum ice sheet thickness: 3367 m. Lowest elevation of the ice sheet bed: -555 m. Age of the ice sheet: 2.4 million years.
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