The
role of orography was found to be crucial in determining the precipitation dis-
tribution and amount.
Atmospheric flow over Iceland was simulated for the period January 1961
through June 2006 using version 3–7–3 of the PSU/NCAR MM5 mesoscale
model (Grell et al., 1995). The domain used is 123× 95 points, centered at
64◦ N and 19.5◦ W, with a horizontal resolution of 8 km. There are 23 vertical
/media/ces/Paper-Olafur-Rognvaldsson_91.pdf
research
VIII. Resources: extensive vs limited
IX. Institutional conditions: open vs constrained
C Scenario content - complex vs simple:
X. Temporal nature: chain vs snapshot
XI. Variables: heterogeneous vs homogenous
XII. Dynamics: peripheral vs trend
XIII. Level of deviation: alternative vs conventional
XIV. Level of integration: high vs low
Scenarios - types
EXAMPLE 1 – EXPLORATORY SCENARIOS
/media/loftslag/Kok_2-scenarios-lecture-2.pdf
BIOMATH, Ghent University, Gent, Belgium
d Water Quality Modelling modelEAU, University Laval, Quebec, Canada
Received 20 December 2005; received in revised form 5 February 2007; accepted 7 February 2007
Available online 27 April 2007
Abstract
A terminology and typology of uncertainty is presented together with a framework for the modelling process, its interaction with the broader
water
/media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.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
Figure 2.3. An overview of the Geysir region. ..................................................................... 20
Figure 2.4 Testing different values for maximum group size in area A1. ............................ 23
Figure 2.5. Testing different values for maximum group size in area A1. ........................... 24
Figure 2.6. A map showing relative locations in box A1 for maximum
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
striking
westwards and a group of N-S-striking pressure axis dipping 45 degrees from the
horizontal and more, suggesting that extensional forces play a large role. Figure 9 includes
the mechanisms of 82 out of the 99 earthquakes in total located between 17 and 26 km
depth and thus shows nearly the same results as described earlier for that interval, that the
tension axis is chiefly horizontal
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf
conditions as a lower
boundary condition from the driving GCM. The RCAO model-output is from a pan-arctic
run for the years 1960–2080 at approx. 50 km resolution. The first 20 years of the model run
must be considered as spin-up time for the ocean module. The RCAO run is experimental
since the model is in a development state and the output has not yet been evaluated over
Greenland (Ralf Döscher, personal
/media/ces/ces_geus_paakitsoq_full_report.pdf
is formed by glacial deposits. The average depth is 5 meters and the residence time
of water in the fjord is about 20 days. As to tidal variations the amplitude is about 0.4 meters. Horsens
fjord consists of marine coastal ecosystems. There are three fairly large islands with cultivated land and
scattered habitation. One of the most important plant community on the islands are along the East coast
/media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf
is formed by glacial deposits. The average depth is 5 meters and the residence time
of water in the fjord is about 20 days. As to tidal variations the amplitude is about 0.4 meters. Horsens
fjord consists of marine coastal ecosystems. There are three fairly large islands with cultivated land and
scattered habitation. One of the most important plant community on the islands are along the East coast
/media/loftslag/Case_A___Horsens_Fjord.pdf