- NIC
Danish Center for Remote Sensing
Canadian Ice Service
Arctic and Antarctic Research Institute - AARI
Norwegian Meteorological Institute
/sea-ice/sea/
Melting Permafrost
Niche Technologies
(Flexible systems)
Med-Long Term
Increased Debris
(Niche Removal
Technology)
Short to Long Term
Remote Sensing
(Nich and Existing
Technologies)
Short to Long Term
Rainfall Management
Niche Technologoes
(Porisoty, skid control)
Short – Long term
Material Composition Physical
Properties
(New mix, recycling, Testing)
Spring Flooding
(Adaptation Tech-
short-long
/media/loftslag/Group4-Pres.pdf
methods be developed to improve monitoring of eruption clouds
in Iceland and in other places where winter-time, with very little sunlight,
and remote and dusty conditions, have a huge impact on the collection of
ground-based data. Gases released during the eruption were
released from magma that erupted; from non-erupted magma; and from the Holuhraun
lava field during and after emplacement
/about-imo/news/final-estimates-of-the-emissions-from-the-holuhraun-eruption-based-on-ground-based-measurements-now-published
to 1.3 cm over one year. In the spring of 2018, a new fracture running down the western slope of Svínafellsheiði was discovered. Recent analysis of remote sensing data shows that the area between the fractures and the glacier margin has moved at a rate of 2 to 4 cm per year in the period from late August 2016 to late August 2017. The area in motion is about 0.5–1 km2 in size. A rough estimate
/about-imo/news/fractures-in-svinafellsheidi-and-a-potential-rockslide-on-svinafellsjokull
from these remote stations are transmitted in real time through wireless connections to the Icelandic Met. Office. The stations are operated and maintained under harsh conditions by IMO's technical team.
The seismic swarm began just outside the northeast caldera rim, but already on the first day the seismicity propagated a few kilometers to the southeast. There it took a sharp bend towards northeast
/about-imo/news/nr/3038
Response of glacier mass balance to regional warming,
deduced by remote sensing on three glaciers in S-Iceland
Sverrir Gudmundsson1, Helgi Björnsson1, Eyjólfur Magnússon1, Etienne Berthier2,
Finnur Pálsson1, Magnús T. Gudmundsson1, Thórdís Högnadóttir1 and Jørgen Dall3
1Institute of Earth Sciences, University of Iceland
/media/ces/glacier_mass_balance_poster.pdf
at
remote places to other people (Gattig & Hendrickx, 2007)
• Different types - Techno-human (e.g. pollution from cars), natural
(e.g. earthquakes), and every day-life risks (e.g. noise) (Walsh-
Daneshmandi & MacLachlan, 2000)
• Comparative optimism - People believe they are less likely to be
affected by different environmental risks compared to others (Pahl
et al. 2005; Costa-Font et al
/media/loftslag/Eriksson_1-Risk-perception.pdf
terrestrial lidar to understand the mechanisms driving melt pond evolution on sea ice in the Canadian Arctic
Hans-Gerd Maas and Ellen Schwalbe, TU Dresden, Institute of Photogrammetry and Remote Sensing, Germany. 3D velocity fields at Jacobshavn Isbrae glacier from multi-temporal terrestrial laser scanner data
Lunch 12:30–13:30
Thursday, 13:30–15:00 ‒ Process studies – II
Kjetil Melvold and Thomas
/lidar/lidar-2013/program/
6University of Washington,
Seattle, WA 98195, USA. 7NOAA Geophysical Fluid
Dynamics Laboratory, Princeton, NJ 08540, USA.
*Author for correspondence. E-mail: cmilly@usgs.gov.
An uncertain future challenges water planners.
Published by AAAS
on July 12, 201
1
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/media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf