the validity of the ideal gas law, hydrostatic
balance, a piecewise linear vertical gradient of air temperature, and neglecting the effects of water
vapour. Pressure, p, as a function of height can then be derived through vertical integration of the
hydrostatic balance equation, and is given by
p(h(x;y);z) = p0 exp
g
R
Z h(x;y)+z
0
dx
T (x )
; (5)
where p0 is pressure at mean sea level, T
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
A survey on flood risk perception was conducted in the town of Selfoss from May to August 2009 among
the residents aged above 18. The respondents were proposed to draw the boundaries of areas flooded
from the beginning of the 20th century on an orthophotograph of Selfoss at scale 1:10.000. The spatial
representations of the flood area were processed with a regulated grid of 10 x 10 metres
/media/loftslag/Spatial_perception_of_flood_hazard_in_the_urban_area_of_Selfoss,_Iceland.pdf
Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009
ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost
operating manage- ment develop- poned-, of land grants ons European tax over- level
costs ment ment comprehen- build- and com- Regional De- heads
1991- 1991- sive- and ings pensation
/media/loftslag/Traffc-maintenance_expenditures.pdf
areas
from 3 to 15,000 km2
3 GCM/RCMs (with SRES A1B emissions)
Echam5/HIRHAM5
BCM/RCA3
HadCM3Qref/HIRHAM
2 Methods for transferring RCM output
to 1 x 1 km grid
Delta change
Empirical adjustment method (met.no)
25 calibrated hydrological models
for 115 catchments
Flood frequency analysis for
200-year flood
⇒ Construct pdfs from
150 results for each catchment
Viksvatn (Hestadfjord) - 83.2
IS92a
/media/ces/Lawrence_Deborah_CES_2010.pdf
with 20% and 2% for the HIRHAM experiments
using HadAM3H and with 30% and 7% for the ECHAM-
driven experiments for Middle Europe and Scandinavia,
respectively.
[18] RCM output is not available for the entire period
1961–2100 because transient RCM simulations are com-
putationally very demanding. Instead two 30-year time
slices are available; one representative for the climate in
the period 1961–1990
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
emission will be monitored closely and forecasts issued if needed.
From the Icelandic Met Office: The Aviation Colour Code for Bárðarbunga is now yellow.
The next meeting will be held on Tuesday 10th of March 2015.
The National Commissioner of the Icelandic Police, Department of Civil Protection and Emergency Management
Almannavarnir www.avd.is/en Twitter: @almannavarnir
/media/jar/Factsheet_Bardarbunga_20150303-b.pdf
are now being detected by
Tungnafellsjökul.
From the Icelandic Met Office: The Aviation Colour Code for Bárðarbunga is yellow.
The Scientific Advisory Board will convene when needed.
The National Commissioner of the Icelandic Police, Department of Civil Protection and Emergency Management
Almannavarnir www.avd.is/en Twitter: @almannavarnir
/media/jar/Factsheet_Bardarbunga_20150310.pdf
longitude
• Conversion process from Sunshine Hours
to Solar Irradiation
Data Source: UKCP09 gridded data set observed data (5km x 5km)
UK Solar Resource
present and future
Sunshine Hours to Solar Irradiation
• Suehrcke conversion method
• Performed conversion on each grid cell for
each month of each year from 1961 to 1990
• Averaged the results for each month and
season
Solar Irradiation Monthly
/media/ces/Burnett_Dougal_CES_2010.pdf
with whom a slot is proposed to
be swapped.
In the closing session on Friday afternoon another two Workshop participants will be offered the
opportunity of presenting a brief summary of key impressions and messages (2 x 5 minutes). This will
require some degree of co-ordination among the rapporteurs. The Conference organizers need to know in
time (Friday morning at the latest) who will present
/media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf