≤
≤
>−
0
00
0
)(
TTif
TTifTTDDFsnow
≤
>−
0
00
0
)(
TTif
TTifTTDDFice
Mean annual temperature difference
Difference relative to 1971-2000
Difference between 25% warmest and 25% coldest years
barb2right +1°C (25% warmest)
barb2right -0.7°C (25% coldest)
barb2right +1.7°C
Catchment elevation (m.a.s.l)
Catchment elevation (m.a.s.l)
s
n
o
w
m
e
l
t
(
m
m
/
d
)
g
l
a
c
i
a
l
m
e
l
t
/media/ces/Crochet_Philippe_CES_2010.pdf
-Skaugen, T., Haugen, J.E., & Hanssen-Bauer, I. (2008). Dynamically downscaled climate scenarios available at the Norwegian Meteorological Institute - per December 2008, met.no report 24/2008.
Gregow, H. & Ruosteenoja, K. (2010). Estimating the effect of climate change on surface geostrophic winds in Northern Europe (CES Climate Modelling and Scenarios Deliverable D2.4). Finnish Meteorological
/ces/publications/nr/1680
are tested: Method I (MI) that uses the same flow
law parameter, A, as in the two studies discussed above, im-
plicitly including basal sliding, and Method II (MII) that in-
cludes a Weertman type sliding law (Paterson, 1994) where
the sliding velocity is assumed to be proportional to a power
of the basal shear stress, τb, (Vslid =C · τmb ); C is the slid-
ing parameter and the exponent m= 3 in our
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
....................................... 16
CLIMATE PROJECTIONS
Kjellström, E., Drews, M., Christensen, J.H., Haugen, J.E., Haakenstad, H. and Shkolnik, I.
An ensemble of regional climate change scenarios for the Nordic countries........................................................ 18
Benestad, R.E.
An analysis of simulated and observed storm characteristics
/media/ces/ces-oslo2010_proceedings.pdf
networks for
t
i Christiansen Barlebo
r Voldgade 10, DK-1350 Copenhagen K, Denmark
form 3 May 2007; accepted 11 May 2007
29 June 2007
www.elsevier.com/locate/jenvman
Mak
manage
ARTICLE IN PRESS
brought together to find a solution that is adequate from
multiple perspectives. This, not only requires coping with
various sources and types of uncertainty, but also with the
ambiguity produced
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
of the cryosphere
Reykholt, Iceland, June 20–21, 2013
4
Sessions
Thursday, June 20
09:00‒09:10 ‒ Welcome
09:10‒10:30 ‒ Lidar measurements for glacier inventories and mass balance monitoring
11:00‒12:30 ‒ Process studies - I
13:30‒15:00 ‒ Process studies - II
15:30‒17:30 ‒ Lidar measurements from space, incl. video discussion with input from
NASA/USA
18:30‒20:00 ‒ Workshop dinner
/media/vatnafar/joklar/Reykholt-abstracts.pdf
in sessions organised in conjunction with Arctic Circle by the
World Council of Churches and the Church of Iceland on "Just Peace with
the Earth", Thursday, and "Climate Justice" on Saturday. In both
events he gave a presentation and took part in round table discussions. Bartholomew I patriarch of the Orthodox church also
participated in the latter event.Sigrún Karlsdóttir, director of Natural Hazards
/about-imo/news/imo-at-the-arctic-circle-assembly-2017
movement. The operation of the seismographs was ceased in 1914 due to funding restrictions during World War I.
The operation of the seismographs was recommenced in 1925 and 1927 at the Icelandic Meteorological Office (IMO), where data processing was also conducted. Amplification of ground motion was low and even several felt earthquakes were not recorded. In 1951-1952, three Sprengnether short-period
/earthquakes-and-volcanism/conferences/jsr-2009/100_years/
(i. e. the location of the measuring point at each river) is also available as pdf (7.2 Mb). See Jökulsá á Fjöllum in the northeast, Markarfljót in the south and Haffjarðará in the west. The volcanic eruptions in March, April and May 2010 are shown in red.
Related topics
/hydrology/articles/nr/2110