fields.The glacial retreat has led to significant
changes in hydrological conditions as the course of glacial rivers has been
altered, new pro-glacial lakes have been formed, while existing ones have
become more extensive or, in some cases, dried up. In 2009, the river Skeiðará
altered its course and joined with the river Gígjukvísl, leaving an 880 m long
bridge running over mostly dry riverbed
/climatology/iceland/climate-report
fields.The glacial retreat has led to significant
changes in hydrological conditions as the course of glacial rivers has been
altered, new pro-glacial lakes have been formed, while existing ones have
become more extensive or, in some cases, dried up. In 2009, the river Skeiðará
altered its course and joined with the river Gígjukvísl, leaving an 880 m long
bridge running over mostly dry riverbed
/climatology/iceland/climate-report/
hedged against small
climate changes. Additionally, climate projec-
tions were not considered credible (12, 14).
Recent developments have led us to the
opinion that the time has come to move
beyond the wait-and-see approach. Pro-
jections of runoff changes are bolstered by the
recently demonstrated retrodictive skill of cli-
mate models. The global pattern of observed
annual streamflow trends
/media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf
the impacts of
climate change on Nordic Energy resources and systems. The first project started in 1991 with
a start-up conference in Iceland in 1991. This project was funded by the Nordic Council of
Ministers and was in many ways a front runner of climate impact assessments internationally,
focusing on the Nordic energy sector. In the early 2000s, an initiative by Nordic Energy
Research led/media/ces/ces-oslo2010_proceedings.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
for the time period 2001–2009, obtained from the permanent SIL network, were analysed to
study stress changes associated with the main shocks. Results reveal a coseismic counter-clockwise
rotation of the maximum horizontal stress of 11 ± 10° (95 per cent confidence level) in the main rupture
region. From previous fault models obtained by inversion of geodetic data, we estimate a stress drop/media/norsem/norsem_martin.pdf
than can be expected to originate from the cauldrons, three to four times the wa-
ter equivalent of the accumulation of snow over the watershed of the cauldrons. It has
been estimated that flow from the cauldrons, in addition to the jökulhlaups, could be
2–5 m3 s 1 at maximum (Vatnaskil, 2005). It is possible that part of the sulfate-rich
groundwater from the glacier comes from the cauldrons
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
is the most comprehensive pan-European research Icelandic scientists have led. It seeks to integrate research on volcanic eruptions, monitoring systems, preparedness and response.
Eyjafjallajökull
Fourth day of eruption in Eyjafjallajökull. Ash plume above clouds 17 May 2010 at 21:46. Photo: Ólafur Sigurjónsson, Forsæti III.
Horizon 2020, the EU framework programme for research
/about-imo/arctic/futurevolc/
flood will commence in the coming weeks-months, the water levels under the ice will drop yet there will not be an eruption (as in 2010).A glacial flood will commence in the coming weeks-months, the water levels under the ice will drop and Grímsvötn will erupt. It is most likely that the eruption will be small to medium-sized with significant volcanic tephra fall on Vatnajökull glacier and little
/about-imo/news/the-civil-protection-scientific-advisory-board-meets-to-discuss-the-status-of-grimsvotn