a coherent, emergent signal in RSAM data (see Figure
2), raising the question: Can RSAM data be empirically used to detect volcanic tremor events
preceding eruptions?
6
Figure 1. Photo of the monitoring setup in the IMO’s natural hazards monitoring room. The
right screen shows real-time earthquake and tremor data. Tremv output is displayed in red
box with the last 24 hrs of all frequency
/media/vedurstofan-utgafa-2021/VI_2021_008.pdf
ENSEMBLES ensemble, in a grid
box in western Norway. As expected, the local changes tend to increase with the large-scale
changes. However, as generally turns out to be the case, this relationship is much tighter for
temperature (the large-scale change explains 86% of the variance of the local change) than for
precipitation (only 40% of the variance of the local change is explained5
/media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf
Baldur Ragnarsson 30.4.2008
As customary in most European countries, Icelanders measure temperatures in degrees Celsius. Here is a handy temperature conversion that can be used to convert degrees Fahrenheit to degrees Celsius and vice versa. Enter a number in either field, then click outside the text box.
Fahrenheit:
Celsius
/weather/articles/nr/1285
Publications on behalf of the European Geosciences Union.
962 G. Aðalgeirsdóttir et al.: 20th and 21st century evolution of Hoffellsjökull glacier
2006) is used to simulate the evolution of Hoffellsjökull out-
let glacier of the Vatnajökull ice cap. The model is run
from the Little Ice Age maximum extent, at the end of the
19th century, throughout the 20th century and then used to
predict the future
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
including, for example, ensuring dam safety. The
goal of the new Climate and Energy Systems project is to look at climate impacts closer in time and assess the
a n o ect ves o t e ro ect
An evaluation of risk under increased uncertainty in
order to improve decision making in a changing
climate was carried out through the following steps:
development of the Nordic electricity system for the next
/media/ces/ces_risk_flyer.pdf
and surveillance of earth, water
and air showed its strength and was in particular very helpful in
the pro vision of gas-distribution forecasts for the public. All divi-
sions of IMO contributed to the e?ort which was carried out in
close co-operation with the University of Iceland and the Civil
Protection in Iceland, with great backing from our ministry and
the government.
It is not enough
/media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
Veðurstofa Íslands
2 Almannavarnadeild Ríkislögreglustjóra
3 Jarðvísindastofnun Háskólans
4 Istituto Nazionale di Geofisica e Vulcanologia (INGV), Bologna
5 Istituto Nazionale di Geofisica e Vulcanologia (INGV), Pisa
6 Jarðvísindadeild Háskóla Íslands
7 Agricultural University of Iceland
8 Consultant
Skýrsla nr. Dags. ISSN Opin Lokuð
VÍ 2020-011 Desember 2020 1670-8261 Skilmálar:
Heiti skýrslu
/media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf
)
is shown. At the margin the grid boxes of the RCAO RCM are
visible. The area between Illulisat and Swiss camp is commonly
called Paakitsôq.
respectively. The Automatic Weather Stations (AWS) Swiss Camp and Crawford are located
on the ice sheet and are operated by the Greenland Climate Network (GC-net) (Steffen and
Box, 2001). The locations of the stations are indicated in Fig. 1, further details
/media/ces/ces_geus_paakitsoq_full_report.pdf
to changing climate conditions. This includes changes in
production modes and infrastructure. In the third set of socio economic conditions the society is willing to
change their lifestyle, which allows the implementation of adaptive measurements which can be
considered as out of the box solutions, e.g. abandoning agriculture completely. In general in all three socio
economic condition sets
/media/loftslag/Group2-report.pdf