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
-based forecast and the text forecast for a specific area, then the text forecast applies.
Keep in mind that short-term forecasts are more likely to be correct than long-term forecasts.
The sliding bar beneath the map is used to view the various forecast periods. It is possible to click on the sliding bar, the days, the hours, or the arrows at the either end of the bar. Additionally, the left
/weather/articles/nr/1210
these fractures will slip if their Coulomb failure stress (CFS) exceeds zero. Thus
the shear stresses are limited by frictional sliding on the numerous fractures.
Cook (1981) studied the behaviour of frictional sliding of granitic rock by use of stiff laboratory
machines. The availability of stiff machines made it possible to study not only the sudden unstable slips
(produced by less
/media/norsem/norsem_slunga.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
heavy rain
5.4
July 2014 Árnestindur, Trékyllisvík in
Strandir
A few days of heavy rain prior
to the slide, permafrost in the
starting area
0.3
July 2014 Askja Snowmelt, sliding surface
connected to faults in the
caldera rim
20
Sep. 2017 Hamarsfjörður Heavy rain 0.8–1
July 2018 Fagraskógarfjall in Hítardalur High ground water pressure
due to long period of rain.
Instability
/media/frettir-myndasafn-2018/Big_landslides_Table_ENG.pdf
mm to 30 mm every six hours. Light and heavy precipitation is represented by light-green and purple shading, respectively.
Atmospheric pressure at the ocean surface is also shown in millibars (1 mb = 1 hPa).
The sliding bar below the map is used to change the validity time of the forecast
It is possible to change the validity time in many ways:
It is possible to click anywhere
/weather/articles/nr/1218
–averaged
modeled ice velocity corresponding to the simulated 2002 ice sur-
face geometry, using A= 6.8× 10−15 s−1 kPa−3 implicitly includ-
ing the basal sliding (in B), and using A= 4.6× 10−15 s−1 kPa−3
and C = 10× 10−15 m a−1 Pa−3 (in (C)). (D) The contribution of
the modeled basal sliding to the velocity shown in (C).
Table 2. Average annual (September 2002 to September 2003;
accuracy ∼2 m a−1
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
shows the direction of the wind, which blows toward the point of the barb. Wind-speed is symbolized by diagonal lines at the end of the barb; for instance, a short line represents 2.5 m/s, a long line 5 m/s and a triangle represents 25 m/s.
Mean sea level pressure is shown in solid lines, the contour interval is 2 hPa.
The sliding bar below the map is used to change the validity time
/weather/articles/nr/1211