14 0 1 2 3 8 12
15 0 1 2 3 8 12
16 0 1 2 4 8 12
17 0 1 2 4 8 12
18 0 1 2 4 8 12
19 0 1 2 4 8 13
20 0 1 2 4 8 13
21 0 2 3 5 9 13
22 1 2 3 5 9 13
23 1 2 3 4 9 13
MEAN 1 2 2 4 8 13
10
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LONGITUDE
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/media/vedur/aerodrome_summaries_20140603.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/
The majority of the grid cells show
no significant change, however a
rising trend towards the end of the
century is noted (red curve).
2071 -2100 relative to 1961-90 [%]
Rossby Centre
i l d l Declines No change Increases
Changes in % for grid cells
with significant changes
Activities and results
reg ona mo e
and ECHAM4
Rossby Centre
regional model
and HadAM3
ECHAM4: A2 0.1 73.2 26.7
ECHAM4: B2 0.1
/media/ces/ces_wind_flyer-hq.pdf
fatalities occurred in
mobile homes,
although only 7.6% of
U.S. housing units in
2000.
• A one standard
deviation in the
proportion of mobile
homes in housing stock
(8.3 percentage
points) increases
fatalities by 36% and
injuries by 18%.
The Mobile Home Problem
50
60
70
80
90
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/media/loftslag/Tornado_Impacts_-_FMI_Presentation.pdf
in Finland
Noora Veijalainen a,*, Eliisa Lotsari b, Petteri Alho b, Bertel Vehviläinen a, Jukka Käyhkö b
a Freshwater Centre, Finnish Environment Institute, Mechelininkatu 34a, P.O. Box 140, FI-00251, Helsinki, Finland
b Department of Geography, FI-20014 University of Turku, Turku, Finland
a r t i c l e i n f o
Article history:
Received 7 January 2010
Received in revised form 13 June 2010
Accepted
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
were carried out to obtain the flow and
sliding parameters for Hoffellsjökull that resulted in a good
simulation of the observed 20th century evolution of the
glacier geometry. The obtained values for the rate factor
and the sliding parameter are A= 4.6× 10−15 s−1 kPa−3 and
C = 10× 10−15 m a−1 Pa−3, respectively.
The ice divide is kept at a fixed location in the model com-
putations presented here
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
by season (%) between
1991-2007 and 1961-1990 in the Baltic countries
1
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/media/ces/ces_SA_group_flyer_new.pdf
Neotectonics in Nordland; NEONOR 2
C. Lindholm, O. Olesen, I. Janutyte, S. Gradman, M. Keiding, H. Kierulf,
M. Ask, J. Dehls, Y. Maystrenko, F. Riis, L. Rise and other project partners
The Nordland shore region is known to be seismically active with deep local sediment basins on the
continental shelf that stretches some 200 km west of the coastline. The offshore areas west of Nordland
have
/media/norsem/norsem_lindholm.pdf
h
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/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf