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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/
Office:
Valid:
Analysis
00 z
06 z
12 z
18 z
Forecast
00 z
06 z
12 z
18 z
SIGWX charts:
Valid:
NAT
00 z
06 z
12 z
18 z
EUR
00 z
06 z
12 z
18 z
EUR wind forecast charts
NAT wind forecast charts
Tropopause - height and temperature
Max wind and FL
Humidity
/weather/aviation/wafc/
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
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no
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e
problem
si
n
th
e
(far
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e
(20
year
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o
r
more
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s
et
al
.(
200
6),
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e
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d
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k
(200
2),
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t
al
.(
199
7)
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s
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n
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rth
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(far
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e
(20
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o
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more
)
Raadgeve
re
t
al
.(
200
8),
Pahl-Wos
te
t
al
.(
2007
c),
Vos
s
et
al
.(
200
6)
13
.Flexibl
e
measures
,
keepin
g
option
s
ope
n
Measure
s
take
n
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w
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r
propose
d
fo
rth
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
et al., 2002).
11
3.2 Flood frequency distribution and parameter estimation method
The Generalized Extreme Value (GEV) distribution (Jenkinson, 1955) was adopted to model the
flood frequency distribution from the AMF series:
Q(D;T ) =
e+ ak (1 [ ln(1 1=T )]
k) if k 6= 0
e aln( ln(1 1=T )) if k= 0
(3)
where e is the location parameter, a is the scale parameter and k is the shape parameter
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
sr
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ed
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ag
ric
ul
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re
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ar
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inatin
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/media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf
). This can be helpful with respect to
finding a common structure in presenting as well in session reporting (for which angles
mentioned in the opening session statements of the Workshop participants can provide
checkpoints).”
Session rapporteur allocation
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.
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/media/loftslag/Guidelines2-for-rapporteurs.pdf