of
temperature anomaly
(ºC) between 1991-2007
and 1961-1990
Variation of annual T
anomaly (ºC)
between 1991-2007
and 1961-1990
Seasonal differences of P
anomaly (in %)
between 1991-2007 and
1961-1990
Seasonal differences of Q
anomaly (in %) between
1991-2007 and 1961-1990
Variation of annual P and Q
anomaly (%)
between 1991-2007
and 1961-1990
-40
-25
-10
5
20
35
50
1
9
2
0
1
9
4
0
1
9
6
/media/ces/Kriauciuniene_Jurate_CES_2010.pdf
series analysis
Regional series are compiled based on regions
having similar climatological characteristics and
streamflow regimes. These series are also useful
for evaluating patterns and trends, both in time and
by region. Regional series for precipitation,
temperature and runoff are being compiled,
updated and analysed within the CES project.
-
4
0
-
2
0
0
2
0
4
0
6
0
W
S
P
S
U
M
A
Q
,
%
-
4
0
/media/ces/ces_SA_group_flyer_new.pdf
0.95
vhm149 1.46
vhm205 1.01
vhm206 1.28
vhm221 0.9
vhm265 1.16
vhm277 0.87
vhm278 -0.12
18
l
l l l
l
llll
l
llll
lll
ll
lll
lllll
lllll
ll l
l l
l
l
l l
l l
l
l
−2 0 2 4 6
0
1
2
3
4
−ln(−ln(1−1/T))
Q/
E[
Q]
1 2 5 10 20 50 100
T (years)
l
l
l
l
l
l
l
l
vhm148
vhm149
vhm205
vhm206
vhm221
vhm265
vhm277
vhm278
Regional +/− 95% CI
H1 0.995
H2 −0.877
l
l
l
l
l
l l l l
l
l
l l
l
l
l
l
l
l
l
l
l
l
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf
Figure 5. AMF frequency distributions (Q(D;T ) vs. T ) at target sites treated as ungauged,
using best overall index flood model (bµ(D) = q0(AP)q1): vhm59 (top-left), vhm64 (top-
right), vhm66 (bottom-left), vhm102 (bottom-right). Solid black line corresponds to the
reference GEV distribution fitted to the observed AMF sample. Grey shaded region corre-
sponds to the reference 95% CI. Red solid line
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
6
0
20
40
60
80
10
0
12
0
14
0
−ln(−ln(1−1/T))
Q(
T)
(m
?s)
1 2 5 10 20 50 100
T (years)
l Obs.
WaSiM vhm51
heM
95?bh ??Obs
95?bh ??W aSiM
95?bh heM
Annual max. Q : GEV Distributions for vhm51
Index flood model no. 6
l l l l
l
l l l
l l l
l
l
l
l
l
l
l
−2 0 2 4 6
0
50
10
0
15
0
−ln(−ln(1−1/T))
Q(
T)
(m
?s)
1 2 5 10 20 50 100
T (years)
l Obs.
WaSiM vhm52
heM
95?bh Obs
95?bh
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf
We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below:
A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö
A
A: Icelandic abbreviation of East (compass direction, easterly, eastern).
ANA: Icelandic abbreviation of Eastnorthesast (compass direction).
ASA: Icelandic
/weather/articles/nr/1208
We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below:
A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö
A
A: Icelandic abbreviation of East (compass direction, easterly, eastern).
ANA: Icelandic abbreviation of Eastnorthesast (compass direction).
ASA: Icelandic
/weather/articles/nr/1208/
2050s 2080s
C
h
a
n
g
e
i
n
r
a
t
i
n
g
(
%
)
10%
50%
90%
C
h
a
n
g
e
i
n
r
a
t
i
n
g
(
%
)
C
h
a
n
g
e
i
n
r
a
t
i
n
g
(
%
)
Each bar
shows
range over
whole UK
spatial
area
June 2010 13
Is the impact similar over the
whole UK?
• Changes in the summer minimum rating, i.e.
worst-case conditions – max temperature:
Rating at baseline period 1961
/media/ces/Cradden_Lucy_CES_2010.pdf
M
(171FT
)
FRE
Q
UENCIE
S
(PE
R
CENT
)
O
F
OCCU
R
RENC
E
O
F
CONCURREN
T
WIN
D
DIRECTIO
N
(I
N
30
0
SEC
T
ORS
)
AN
D
SPEE
D
(I
N
KN
O
TS
)
WITHI
N
SPECIFIE
D
RANGE
S
ANN
U
A
L
WIN
D
WIN
D
SPEE
D
(KT)
)
DIRECTIO
N
CAL
M
1–
5
6–1
0
11–1
5
16–2
0
21–2
5
26–3
0
31–3
5
36–4
0
41–4
5
46–5
0
>5
0
T
O
T
A
L
V
ARIABL
E
0
0
0
0
0
0
0
0
0
0
0
0
0
35-36-0
1
3
2
3
3
2
1
1
0
0
0
0
0
14
02-03-0
4
0
2
4
4
3
1
0
0
/media/vedur/aerodrome_summaries_20140603.pdf