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dioxide (CO2) is the most important anthropogenic GHG.
Its annual emissions have grown between 1970 and 2004 by about
80%, from 21 to 38 gigatonnes (Gt), and represented 77% of total
anthropogenic GHG emissions in 2004 (Figure 2.1). The rate of
growth of CO2-eq emissions was much higher during the recent
10-year period of 1995-2004 (0.92 GtCO2-eq per year) than during
the previous period of 1970
/media/loftslag/IPPC-2007-ar4_syr.pdf
1998] and RCM output such
as incoming and outgoing, short- and long-wave radiation,
temperature, water vapor pressure, and wind speed:
ETref ¼
0:408D Rn Gð Þ þ g 900T þ 273 u2 es eað Þ
Dþ g 1þ 0:34u2ð Þ ð3Þ
where ETref is reference evapotranspiration (mm d1), Rn is
net radiation at the crop surface (MJ m2 d1), G is soil heat
flux density (MJ m2 d1), T is mean daily air temperature
at 2 m
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
Elvehøy, H., Guðmundsson, S., Hock, R., Machguth, H., Melvold, K., Pálsson, F., Radic, V.,
Sigurðsson, O. and Þorsteinsson, Þ.
The impact of climate change on glaciers and glacial runoff in the Nordic countries .......................................... 38
Radic, V. and Hock, R.
Volume changes of the glaciers in Scandinavia and Iceland in the 21st century
/media/ces/ces-oslo2010_proceedings.pdf
University of Innsbruck, Austria
36 Michael Studinger* NASA Goddard Space Flight Center, USA
37 Guðmundur Valsson National Land Survey of Iceland
38 Christian Wever TopScan GmbH, Germany
39 Ian Willis Scott Polar Res. Inst. (SPRI), Univ. of Cambridge, UK
* Video conference
Lidar measurements of the cryosphere
Reykholt, Iceland, June 20–21, 2013
Andreassen and others 9
Lidar measurements
/media/vatnafar/joklar/Reykholt-abstracts.pdf
(DGPS) equipment
in 2001. Continuous profiles, approximately 1 km apart,
were measured in the accumulation zone and a dense net-
work of point measurements were carried out in the abla-
tion zone. Digital Elevation Models (DEMs) of the surface
and bedrock were created from these data (Fig. 2; Björns-
son and Pálsson, 2004). The estimated errors are at most
1–5 m (bias less than 1 m) for the surface
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
). Meteorological observations carried
out on Storbreen in the summer of 1955 (Liestøl1967) revealed that net radiation is the most impor-tant contributor to the ablation at Storbreen. An au-tomatic weather station (AWS) has bee operatedin the ablation zone of Storbreen since September2001 providing a near-continuous series of meteor-
ology and surface energy balance data. Analysis ofthe first five years
/media/ces/GA_2009_91A_4_Andreassen.pdf
has supported the Safetravel project since its beginning in 2010.
ICE-SAR's office leads the project with the help of many SAR team members as well as others with thorough experience in travelling in Iceland in different conditions. Safetravel is supported by a number of sponsoring companies.
SOS Iceland app
The newest option is SOS Iceland, an app which is easy to use. It can be used
/about-imo/news/nr/2497
project since its beginning in 2010.
ICE-SAR's office leads the project with the help of many SAR team members as well as others with thorough experience in travelling in Iceland in different conditions. Safetravel is supported by a number of sponsoring companies.
112 Iceland app
An option is 112 Iceland, an app which is easy to use. It can be used in emergency, if an accident occurs
/about-imo/news/nr/2707