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
study and location of catchments. Catchment vhm278 is embedded
within vhm148 and catchment vhm277 is embedded within vhm149.
9
l
l l l
l
l
ll
l
l
l
l
l
l l l
l
l l
l
ll l l l
l
l
l ll
l
ll
l
l l
l l
l
0 100 200 300
10
0
20
0
30
0
40
0
Day since 1st Sept.
Q
m³
/s
VHM 148
S O N D J F M A M J J A
l
l
ll l l
l
ll
l
l
l
ll
l
l
ll l
l
0 100 200 300
15
0
25
0
35
0
45
0
Day since 1st Sept.
Q
m³
/s
VHM
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf
A 1x1 km digital elevation model derived from a 500 m DEM (Icelandic Meteorological Of-
fice, National Land Survey of Iceland, Science Institute, University of Iceland, and National
Energy Authority. 2004), a soil map from the Agricultural University of Iceland and a map of
the bedrock geology from the Icelandic Institute of Natural History (Jarðfræðikort af Íslandi -
Berggrunnur - 1:600.000 - NI
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
the index flood µi(D). For gauged sites, µi(D) is estimated by the sample mean
whereas for ungauged sites, µi(D) is estimated indirectly as a function of physiographic and
climatic catchment characteristics (Ci;k):
bµi(D) = f (Ci;k);k = 1;n: (2)
This estimation is usually performed using the power-form equation:
bµi(D) = q0C
q1
i;1C
q2
i;2::::C
qk
i;k:::C
qn
i;n: (3)
where q denotes the vector
/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