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
örugt að fara fyrir Horn í um 10 sml frá landi en það yrði
að hafa góðan útvörð.
Kl.1341, kalla TFB og spyr um ETA í RVK, ETA um kl 1440.
Kl 1305, AIS umferð fyrir N- Horn. Vegna bilunnar í WS 1 var megináhersla lögð á ískönnun í
þessu flugi.
Flugskýrsla TF-SIF
12. desember 2010
Flug nr. 117410.025
Ískönnun.
Meginröndin lá um eftirtalda staði.
1. 67°47.0N 023
/media/hafis/skyrslur_lhg/Isskyrsla_20101212.pdf
ea
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/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
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24
.Decisio
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)
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/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
6University of Washington,
Seattle, WA 98195, USA. 7NOAA Geophysical Fluid
Dynamics Laboratory, Princeton, NJ 08540, USA.
*Author for correspondence. E-mail: cmilly@usgs.gov.
An uncertain future challenges water planners.
Published by AAAS
on July 12, 201
1
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1 FEBRUARY 2008 VOL 319 SCIENCE www.sciencemag.org574
POLICYFORUM
combined with opera-
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/media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf
(ECT)
Working paths and
machinery transportation
+ C
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Plant production and
transportation
Site preparation
a
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n
e
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d
i
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Thinnings/ harvesting
operations
h di
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S ort stance
transportation
Long distance
n
p
u
t
E
m
i
s
Emission calculation tool
transportation
Chipping
s
i
o
n
CO2 balance
14
Energy wood
/media/ces/Alam_Ashraful_CES_2010.pdf
pm
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/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
probably a few meters.
An interactive 3D model of the earthquakes during the magma
intrusion. The di?rent colours represent the activity in time from
16 August to 12 September.
During the magma intrusion, intense earthquake activity related to
subsidence of the Bárðarbunga caldera was located at the caldera
rim. Over 70 earthquakes above magnitude 5 occurred in the first
four months after the onset
/media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf