) storage coefficient of interflow ki; (3) drainage
density d; (4) the fraction of surface runoff from snowmelt; and (5) the recession constant
krec for the decreasing saturated hydraulic conductivity with increasing depth. For the
groundwater flow, adjusted parameters (6–7) are the hydraulic conductivity in the X and Y
direction. The hydraulic conductivity is adjusted in distributed grids unlike
/media/ces/2010_017.pdf
High-resolution regional
climate simulations over Iceland using polar MM5. Mon. Wea. Rev., 133, 3527–
3547.
Buzzi A., Tartaglione N. and Malguzzi P. 1998. Numerical simulations of the
1994 Piedmont flood: Role of orography and moist processes. Mon. Wea. Rev.,
126, 2369–2383.
Chiao, S., Lin Y.-L. and Kaplan M. L. 2004. Numerical study of the orographic
forcing of heavy precipitation during MAP IOP
/media/ces/Paper-Olafur-Rognvaldsson_91.pdf
Use of relatively located micro-
earthquakes to map fault patterns
and estimate the thickness of the
brittle crust in Southwest Iceland
Sigurlaug Hjaltadóttir
VÍ 2010-003
Skýrsla
f l l l dUse o re ative y ocate micro-
earthquakes to map fault patterns
and estimate the thickness of the
brittle crust in Southwest Iceland
Sigurlaug Hjaltadóttir, Veðurstofu Íslands
VÍ 2010-003
ISSN 1670-8261
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
were collected through a mail survey in Sweden,
Acceptability of travel demand managemen
of problem awareness, persona
Louise Erikssona,b,, Jo¨rgen Garvil
aDepartment of Psychology
bTransportation Research Unit
Available onlin
Abstract
y 26 (2006) 15–26
t measures: The importance
norm, freedom, and fairness
la,b, Annika M. Nordlunda,b
a˚ University, Sweden
Umea˚ University, Sweden
14 July 2006
/media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf
on the quantity at hand (strengths and weaknesses in
Box 1. The error propagation equation
The error propagation equations for the most common
operators are (s is the standard deviation):
Addition and Subtraction: z ¼ x þ yþ/ or z ¼
x y/
sz ¼
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
s2x
þ
s2y
þ/
r
Multiplication by an exact number: z
/media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
climate changes between the CMIP3 and ENSEMBLES
simulations 15
4. Impact of RCM data on forecasts of climate change 18
5. Probabilistic projections of temperature and precipitation change 24
5.1 Best estimates and uncertainty ranges of temperature and precipitation change 24
5.2 How probably will temperature increase (precipitation change) by at least X°C (Y%)?
28
6. Conclusions 34
References
/media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf
from the glacier margins). This
was done by shifting the x and y coordinates of the
40 m40 m DEMs in 5 m steps and calculating the
correlation to the corresponding values of the 5 m5 m
EMISAR DEM. In all cases, both the maximum correla-
tion and minimum standard deviation yielded the same
shift. After the co-registration, the same ice-free areas
were used to correct the vertical offset of the DMA
/media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
moment release is observed before the onset of the fissure eruption (red bar), i.e. while the dyke was growing, and the moment release in the dyke is now 10,000 times less than it was before the eruption (logaritmic scale on y-axis).
For the caldera (lower panels), things are a bit more complicated, although a clear trend of decreasing activity is found there as well. Most moment is released during
/earthquakes-and-volcanism/articles/nr/3055