14 0 1 2 3 8 12
15 0 1 2 3 8 12
16 0 1 2 4 8 12
17 0 1 2 4 8 12
18 0 1 2 4 8 12
19 0 1 2 4 8 13
20 0 1 2 4 8 13
21 0 2 3 5 9 13
22 1 2 3 5 9 13
23 1 2 3 4 9 13
MEAN 1 2 2 4 8 13
10
AE
R
OD
R
OM
E
CLIM
A
T
OLOGICA
L
SUMMA
R
Y
-
T
ABL
E
D
AE
R
OD
R
OME
:BIK
F
-
KEFL
A
VÍ
K
/K
efl
avi
k
PERIO
D
O
F
RECORD
:2001–201
0
L
A
TITUDE
:6
3
59’06"
N
LONGITUDE
:2
2
36’20"
W
ELE
V
A
TIO
N
AB
O
V
E
MSL
:5
2
/media/vedur/aerodrome_summaries_20140603.pdf
polarity reversal from winter to summer in 2010
and its relation to extreme hot summer associated with polar jet,
summer AO and blocking - Y Tachibana
Group Discussion
10:30 – 11:00 Coffee Break
11:00 – 12:00
11:00 – 11:20
11:20 – 11:40
11:40 – 12:00
12:00 – 12:30
Potential Arctic / Mid-Latitude Linkages – Large Scale (Chair: Jim Overland)
Large scale linkages between fall
/media/loftslag/Mid-Latitudes-Agenda1_nov2013EH.pdf
and corrected data
-5 0 5 10 15
1
.
0
1
.
5
2
.
0
2
.
5
3
.
0
3
.
5
Temperature,°C
P
r
e
c
i
p
i
t
a
t
i
o
n
,
m
m
/
d
a
y
Jan
Feb Mar
Apr
May
Jun
JulAug
Sep
OctNov
Dec
Year
obs ALUKSNE
DMI 1961-1990 ALUKSNE
mod DMI 1961-1990 ALUKSNE
JanFeb
Mar
Apr
May
Jun
Jul
AugSep
Oct
Nov
Dec
Year
Jan
Feb
ar
Apr
May
Jun
Jul
Aug
Sep
Nov
Dec ear
After the
correction all 3
climate models
agree with
observed data
/media/ces/Kurpniece_Liga_CES_2010.pdf
for
behavioural responses to policy
• Psychological models of behaviour change (e.g., TPB)
Ajzen & Fishbein (1991)
Subjective
norm
Specific
attitudes
Perceived
behavioural
control
Intention Behaviour
Normative
beliefs
Behavioural
beliefs
Control
beliefs
P
O
L
I
C
Y
(3) Factors important for
behavioural responses to policy cont.
• Cost-minimization principle (Loukopoulos et al. 2006)
• Barriers
/media/loftslag/Eriksson_2-Acceptability-of-policy.pdf
is first derived (Figure 3, left). The cumulative area distribution function S(s) (shown
on the x-axis) represents total area of all glaciers with area less than s (shown on the y-axis
of the figure). Typically, the total glaciated area and an estimate of the area of a few of the
TóJ 4 5.12.2009
Memo
a71
a71a71
a71
Area (km2)
Volume
(km
3 )
10 103 105 107
1
10
2
10
4
10
6
Icelandic ice caps, v
/media/ces/ces-glacier-scaling-memo2009-01.pdf
Journal of Social Issues, 56, 407-424.
Von Korff Y, d'Aquino P, Daniell KA, Bijlsma R (2010) Designing participation processes for water management and beyond. Ecology and Society 15(3): 1.
http://www.ecologyandsociety.org/vol15/iss3/art1/
Samuelson CD (1993). A multiattribute evaluation approach to structural change in resource dilemmas. Organizational Behavior and Human Decision Processes
/media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf
the validity of the ideal gas law, hydrostatic
balance, a piecewise linear vertical gradient of air temperature, and neglecting the effects of water
vapour. Pressure, p, as a function of height can then be derived through vertical integration of the
hydrostatic balance equation, and is given by
p(h(x;y);z) = p0 exp
g
R
Z h(x;y)+z
0
dx
T (x )
; (5)
where p0 is pressure at mean sea level, T
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
750-1170
AAR of the warm year of 2004
- digitized using the October 2004 SPOT 5 HRS images
Ice cap
E: Eyjafjallajökull
To: Torfajökull
Ti: Tindfjallajökull
AAR (%)
20-25
<5
0
Method
References
Berthier E., Arnaud Y., Baratoux D., Vincent C. and Rémy F. 2004. Recent rapid thinning of the "Mer de Glace" glacier derived from satellite optical images.
Geophys. Res. Lett., 31, L17401, doi:10.1029
/media/ces/glacier_mass_balance_poster.pdf
and the y-axis the dates between March and July. For every year,
the melt season starting date is plotted (blue dots), and a blue line connects the dates for all the
years. A regression line fitting those values (orange line) is shown, and the difference in days
between the beginning and the end of the period, as calculated from the regression line, is
indicated at the top of the plot.
In 9 cases
/media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf