Discussion on weighing factors might hamper
the creative process.
• Being concrete requires expert opinions. Especially when developing a FCM
from scratch requires a high level of understanding of all participants.
Further reading
Kok, K. 2009. The potential of Fuzzy Cognitive Maps for semi-quantitative scenario development, with an example from
Brazil. Global Environmental Change 19: 122-133
Van
/media/loftslag/Kok_2-scenarios-lecture-2.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
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/
tunnisteväriSeuraukset
Scenario probability high
ACT
MONITOR
Consequence
probabi lity low
after control
methods
PREPARE
PREPARE
Scenario probability low
Consequence
probabili ty high
after control
methods
Likely
Very unl ikely
Very likely
Virtuall y certain
Unlikely
V
e
r
y
l
i
k
e
l
y
L
i
k
e
l
y
V
e
r
y
u
n
l
i
k
e
l
y
Excepti onally unlikely
= major consequences
= moder ate consequences
= minor
/media/ces/Keranen_Jaana_CES_2010.pdf
downscaling
results previously obtained by Kaas (1993, 1994), as well as results from four different climate
models (with the GFDL CM3 as the primary reference). The study found a warming of 0.3 K
per decade until the middle of the 21st Century, with a wintertime warming rate of 0.35 K per
decade, and a warming rate of 0.25 K per decade in summer. The study also examined precipitation
changes and found
/media/ces/2010_005_.pdf
A reduction in the glaciated area at the
lowest altitudes is specified as
DSa1 = kDSa ; (10)
where k is an adjustable parameter, 0 < k < 1. This reduction is carried out by eliminating
the ice-cover sequentially, starting with the lowest elevation band or grid cell of the group and
continuing upward until the total eliminated ice-covered area is equal to DS1. Some ice may
remain in the uppermost
/media/ces/ces-glacier-scaling-memo2009-01.pdf
of Iceland.
After registration at 09:00, an opening address will be given by Pétur K. Maack, Director General of Icelandic CAA, at 09:30. Lectures and disscussions will take place until summary at 16:30.
The full programme is available as pdf (55 Kb) but the various topics come under these main headings:
Ash measurements, experience 2010 and 2011
Initial and boundary data acquisition
/about-imo/news/nr/2421
15.0W
9) 67 05.0N 21 52.0W
10) 66 57.0N 22 32.0W
11) 67 00.0N 23 00.0W
12) 66 38.0N 25 00.0W
13) 66 30.0N 26 40.0W
Næst landi var ísinn á eftirfarandi stöðum:
1. 48 sjml vnv af Grímsey.
2. 46 sjml ana af Horni.
3. 34 sjml norður af Skagatá.
4. 25 sjml nnv af Sraumnesi.
Kl 0003 Kallað í Remoy Viking k/m LLDM til að fá upplýsingar um ísinn sem hann er að
sigla í gegnum
/media/hafis/skyrslur_lhg/isskyrsla_14122010.pdf
K. Maack, Director General Icelandic CAA
Ash measurements, experience 2010 and 2011
9:45 Eruptions in Eyjafjallajökull, Etna and Grímsvötn, airborne OPC measurements and quality
assurance Konradin Weber, UAS, Düsseldorf Germany
10:15 Observations in plumes and vicinity of airports Jonas Eliasson HÍ (UI)
Initial and boundary data acquisition and improvements in modelling
10:45
/media/vedurstofan/utgafa/hlidarefni/program17012012.pdf