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line shows the number of all measured earthquakes but the red line shows the number of earthquakes above 1.5 in magnitude.
During these years, the measuring net has improved and become more sensitive. That is the reason for showing the larger earthquakes separately.
18 August 2014 20:45 - An overview of the first three days
Since the onset of the earthquake swarm at Bárðarbunga on Saturday
/earthquakes-and-volcanism/articles/nr/3000
–5
months per year depending on watershed. Mean yearly maximum snow thickness
decreases by 0–80%.
Winter flow is predicted to increase on average due to a higher number of melt events at
relatively high and flat heath areas of the watersheds. For Sandá í Þistilfirði, vhm 26, the
snowmelt generated spring/summer discharge peak largely disappears and the seasonal
discharge becomes more evenly
/media/ces/2010_016.pdf
of radiation are
added to a classic degree-day model. For infiltration, a methodology of Peschke, based on
the approach of Green and Ampt, was used. To calculate the fluxes within the unsaturated
soil zone, the Richards equation was used. The groundwater table was modelled in both the
unsaturated zone module and the groundwater module. The coupling between both modules
was done by a net/media/ces/2010_017.pdf
in 1991. The blue dashed line shows the number of all measured earthquakes
but the red line shows the number of earthquakes above 1.5 in magnitude.
During these years, the measuring net has improved and become more sensitive. That is the
reason for showing the larger earthquakes separately.
18 August 2014 20:45 - An overview of the first three days
Since the onset of the earthquake swarm
/media/jar/Bardarbunga-2014_August-events.pdf
) and are
Global Navigation Satellite System (GNSS) data providers (SONEL, n.d.).
The North Sea is home to one of the most dense tide gauge networks in the world, with over 15 tide
gauge series that span at least 100 years along its coastline (Quante and Colijn, 2016). In Denmark,
17
the national tide gauge network consists of 90 automatic stations run in cooperation of the Danish
Meteorological
/media/vedurstofan-utgafa-2020/VI_2020_005.pdf
and direction, as well as air temperature, from the IMO operational surface station net-
work. Most anemometers are installed at 10 m above ground level (mAGL). However, at some
stations, surface winds are measured at different heights, h, varying between 4.0 and 18.3 m.
3This is done using a GRIB-API command on Parameter 141 (snow depth) in the earliest boundary
data file: grib_set -f -d 0.0 -w
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
line shows the number of all measured earthquakes but the red line shows the number of earthquakes above 1.5 in magnitude.
During these years, the measuring net has improved and become more sensitive. That is the reason for showing the larger earthquakes separately.
18 August 2014 20:45 - An overview of the first three days
Since the onset of the earthquake swarm at Bárðarbunga on Saturday
/earthquakes-and-volcanism/articles/nr/3000/
Summary of the break-out sessions on road infrastructure
By Adriaan Perrels (FMI)
1. Introduction
The break-out sessions, three in total, were interspersed between the various oral presentations
on Thursday afternoon, Friday morning and Friday afternoon. Each session was 60 to 80
minutes. The participants had two assignments:
1. deliberate 7 questions on issues pertaining subsequent
/media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf
in the data used in making the
decision and the factors are interlinked, all of which makes
the problem highly complex. The part of the net defined by
variables and links is relatively easily communicated to
stakeholders (Henriksen et al., 2007b). However the
tal Management 88 (2008) 1025–1036
quantitative part, with the conditional probability tables
(CPTs), the numbers, is the step where
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf