Flugskýrsla TF-SIF
12. desember 2010
Flug nr. 117410.025
Áhöfn:
Flugstjóri Hafsteinn Heiðarsson
Flugmaður Jakob Ólafsson
Flugmaður 2 / Þjálfunarfl.
Yfirstýrimaður Auðunn F. Kristinsson
Stýrimaður Gunnar Örn Arnarson
Stýrimaður
Stýrimaður
Aðrir 9 farþegar, 4 til Akureyrar en 5 með allt flugið.
Flugtími:
Flugvöllur Hreyfing Flugtak Flugvöllur Lending
/media/hafis/skyrslur_lhg/Isskyrsla_20101212.pdf
Dashed lines encompass the V-shaped zone of tephra deposition. (c)
Oblique aerial view from west of the tephra plume at Grímsvötn on 2 November. Note the ashfall
from the plume. (Photo by M. J. Roberts.) (d) Weather radar image at 0400 UTC on 2 November.
The top portion shows its projection on an EW-vertical plane. The minimum detection height for
Grímsvötn is seen at 6 km, and the plume extends
/media/jar/myndsafn/2005EO260001.pdf
drainage
works, and land-cover and land-use change.
Two other (sometimes indistinguishable)
challenges to stationarity have been exter-
nally forced, natural climate changes and
low-frequency, internal variability (e.g., the
Atlantic multidecadal oscillation) enhanced
by the slow dynamics of the oceans and ice
sheets (2, 3). Planners have tools to adjust
their analyses for known human distur-
bances
/media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf
ORIGINAL ARTICLE
Climate change adaptation in European river basins
Patrick Huntjens • Claudia Pahl-Wostl •
John Grin
Received: 1 July 2008 / Accepted: 24 December 2009 / Published online: 2 February 2010
The Author(s) 2010. This article is published with open access at Springerlink.com
Abstract This paper contains an assessment and stan-
dardized comparative analysis of the current water man
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
Assessment Re-
port (AR4).
Topic 1 summarises observed changes in climate and their ef-
fects on natural and human systems, regardless of their causes, while
Topic 2 assesses the causes of the observed changes. Topic 3 pre-
sents projections of future climate change and related impacts un-
der different scenarios.
Topic 4 discusses adaptation and mitigation options over the
next few decades
/media/loftslag/IPPC-2007-ar4_syr.pdf
as an
addition to the current scenario development methodology;
to link Fuzzy Cognitive Maps to the concept of resilience, thus
substantiating a major potential strength;
to critically evaluate the strengths and weaknesses of Fuzzy
Cognitive Maps in the context of developing scenarios.
2. Fuzzy Cognitive Mapping
2.1. System dynamics
System dynamics is an umbrella term for all approaches aiming
/media/loftslag/Kok_JGEC658_2009.pdf
-time and
detects signal characteristics similar to previously observed eruptions using a three-fold
detection procedure based on: 1) an amplitude threshold; 2) the signal-to-noise ratio; and 3) an
emergent ramp-like shape. Data from six Icelandic eruptions was used to assess and tune the
module, which can provide 10–15 minutes of warning for Hekla up to over two hours of
warning for some other
/media/vedurstofan-utgafa-2021/VI_2021_008.pdf
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/media/ces/2010_017.pdf