(Percent) By
Year Built Categories
Percent of Homes Damaged By Year Built
Categories
36
24
26
28
30
32
34
Pre 1980 80-9697-2002 Post 2002
Percent Damaged
All Homes – Damage Per Square
Foot
All Homes - Damage Per Square Foot
2
2.5
D
a
m
a
g
e
P
e
r
S
q
.
F
o
o
t
0
0.5
1
1.5
< 120 120-129 130-139 140-149 > 149
D
a
m
a
g
e
P
e
r
S
q
.
F
o
o
t
Pre 1980
1980-1996
1997-2002
Post 2002
/media/loftslag/FMI_-_Disaster_Mitigation.pdf
Thursday, 14 November
Time Agenda Item
09:00 – 10:30
09:00 – 09:20
09:20 – 09:40
09:40 – 10:00
10:00 – 10:30
Potential Arctic / Mid-Latitude Linkages - East Asia (Chair: Jim Overland)
Rapid Arctic Warming in Recent Decades and Its Impact on Climate Change over East Asia
- S-J Kim
Extreme weather in northern mid-latitudes linked to cryosphere loss - Q Tang
A cause of the AO
/media/loftslag/Mid-Latitudes-Agenda1_nov2013EH.pdf
of melt water from glaciated
areas in long integrations for a warming climate.
Glacier dynamics
This problem can be qualitatively analysed by considering the continuity equation for ice vol-
ume, which may be expressed as
¶h
¶t
+
¶q
¶x
= b or
¶h
¶t
+~ ~q = b ; (1)
for a one-dimensional ice flow channel or an ice cap that flows in two horizontal dimensions,
respectively. h is ice thickness, q or ~q/media/ces/ces-glacier-scaling-memo2009-01.pdf
a precipitation value from a given location based on values
from a regular gridded dataset. ................................................................................................. 28
Figure 7. Scatterplots and Q–Q plots comparing daily precipitation from the ICRA dataset and
observations with different extraction methods for station Eskifjörður. .................................. 30
/media/vedurstofan-utgafa-2020/VI_2020_008.pdf
indicate a warming of climate that is
largest in winter and increases from the Atlantic Ocean towards the Arctic Ocean and
northern Russia. This warming is quite large compared with natural interdecadal temperature
variability. Thus, with the exception of the North Atlantic area, there is already during the
decade 2011-2020 at least a 95% probability that the 10-year annual mean temperature
/media/ces/raisanen_ruosteenoja_CES_D2.2.pdf
J A
0 100 200 30020
0
60
0
100
0
Days since Sept. 1st
Q
(m
^3
/s)
Obs
Pred−nearest
Pred−weight
Method 4 T+2: RMSE−nearest= 69.6 RMSE−weight= 44.5
S O N D J F M A M J J A
Figure 7. Observed and predicted daily discharges at vhm 64 for a forecast range (T) of 2 days
and water-year 2004–2005, using methods 1 to 4 with rescaling. The 80%, 90% and 95% pre-
diction intervals are represented by grey
/media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf
A second, but usually smaller, increase in runoff oc-
curs in the autumn. In northern Finland more than 95% of annual
maximum floods are caused by spring snowmelt (cf. Fig. 7a). Also
the small upstream lakes in the northern part of the lake area
and the northernmost of the coastal rivers fall mainly into this cat-
egory. In most coastal rivers the major floods can be caused by
either snowmelt
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
andEnergy Directorate (NVE), Oslo, Norway2Department of Geosciences, University of Oslo, Norway3Institute for Marine and Atmospheric Research, Utrecht University, Utrecht, the Netherlands
Andreassen, L. and Oerlemans, J., 2009: Modelling long-term
summer and winter balances and the climate sensitivity of Stor-breen, Norway. Geogr. Ann. 91 A (4): 233–251.
ABSTRACT. Measurements of winter balance (bw
/media/ces/GA_2009_91A_4_Andreassen.pdf
A A SM J J O N D J F M A A SM J J O N D J F M A A SM J J O N D
J F M A A SM J J O N D J F M A A SM J J O N D J F M A A SM J J O N D
2010–39
(a) (b)
93.
0
93.
5
94.
0
94.
5
2040–69
Lake Pielinen
93.
0
93.
5
94.
0
94.
5
2070–99
94.
5
95.
5
96.
5
2010–39
94.
5
95.
5
96.
5
2040–69
Lake Syväri
94.
5
95.
5
96.
5
2070–99
75.
4
75.
8
76.
2
76.
6
2010–39
75.
4
75.
8
76.
2
76.
6
2040–69
Lake Saimaa
75.
4
75
/media/ces/Water_resources_man_Veijalainen_etal.pdf
19 CMIP3 GCMs are used (Table 2.1). The horizontal grid spacing of these
models varies from 1.1 q latitude × 1.1 q longitude to 4 q latitude × 5 q longitude. For each
2 Some of the RCM simulations in the ENSEMBLES data base were conducted with funding from other sources,
including CES.
5
model, a 198-year time series (1901-2098) obtained
/media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf