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
each time. Both are fully analysed to check for congruity.
Ambient air pumped for an hour into a ~10 litre aluminium container, thereby collecting a compressed sample of great volume, done weekly or semi-monthly depending on season. Various components are analysed, investigating the stability of atmospheric composition.
Twenty-four-hour samples of airborne particles blown from the sea
/pollution-and-radiation/pollution/components/
the largest in North America from 1971
square4 Watershed 177,000 km²
square4 3,000 km of new roads
square4 7 transmissions lines + 7,000 km(735 kV)
square4 9 reservoirs, total area ± 14,000 km2
square4 9 power plants : 16,500 MW
square4 +2 under construction: 17,500 MW
square4 A first and a last
A
La Grande-2 and La Grande-2A
Electricity Consumption / Capita
( kWh, 2005)
Aluminium (90
/media/ces/Demers_Claude_CES_2010.pdf
the past 2 decades. Summer ablation was found to be less than 50% of the 1995 - 2014 average.
Fig. 3 (enlarge). Ablation stake (white) near the northern margin of Hofsjökull on October 9th 2015 at a height of 980 m. A yellow indicator gives the height of the aluminium stake, whereas the red bar shows the typical stake height during years with negative mass balance. Photo: Bergur Einarsson
/about-imo/news/nr/3229
Hoffellsjökull
Gögn/Data: VÍ/IMO, JH/IES
Við Jökulsárlón má sjá hversu mikil áhrif kelng í sjó fram og í jökullón hefur á afkomu jökla. Jök ul sárlón byrjaði að
myndast um . Það er nú ásamt Breiðárlóni og nokkrum öðrum minni lónum við jaðar Breiða merk urjökuls yr km að at ar máli. Síð ustu árin hafa lónin samtals stækk að um
,– km ár lega að meðaltali
/media/Eplicanámskeið/VAT_newsletter_2018_06.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
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-
tions
/media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf