from 5
years of continuous GPS measurements in
Iceland, submitted to Journal of Geophysical
VOLUME 86 NUMBER 26
28 JUNE 2005
PAGES 245–252
Eos, Vol. 86, No. 26, 28 June 2005
EOS, TRANSACTIONS, AMERICAN GEOPHYSICAL UNION
PAGES 245, 248
Forecasting and Monitoring a
Subglacial Eruption in Iceland
Fig. 1. (a) Map of Iceland illustrating the location of monitoring networks discussed in the text
/media/jar/myndsafn/2005EO260001.pdf
and glaciers. The former trend is mainly visible in the
Westfjords, an area in northwest Iceland, in the winter (see Figure 8a and 8b) and in northeast
Iceland in the summer, especially east of Akureyri in the RCP8.5 scenario (see Figures 8c
and d). The latter trend is most clearly seen during summer and in cases with the RCM RCA4
with RCP8.5.
Extreme temperature trends
In a previous section we
/media/vedurstofan-utgafa-2017/VI_2017_009.pdf
mass balance of three small ice caps (with areas from 15 to 80 km2) over 6 to
20 years, were efficiently estimated from maps of glacier elevation changes deduced by SPOT
5 HRS, EMISAR and aerial photographs
• Accuracy of estimating the elevation changes, was greatly improved by using the highly precise
EMISAR DEM as a reference for co-registration and offset correction
EMISAR
Co-registration
/media/ces/glacier_mass_balance_poster.pdf
on the afternoon of Friday,
27 August 2010 (at a time that enables catching late return flights to Norway and Denmark).
Day one: 26 August 2010
9:00 opening and welcome by local representative Sigrún Karlsdóttir and by Adriaan Perrels (FMI, Fi) as NONAM coordinator
9:20 p1 Jens Christian Refsgaard (GEUS, Dk). Uncertainty and Risk - terminology and concepts
9:50 p2 Gareth James Lloyd (DHI, Dk). What
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