/terminology-2009-eng.html
Mitchell J.K. (ed. 1996): The long road to recovery: Community
responses to industrial disasters. UN University Press, 307 p.
Mitchell J.K. (ed. 1999): Crucibles of hazards: Mega-cities and
disasters in transition. UN University Press, 535 p.
WMO/trj
Observations
Inventory
Accounting
Thematic event maps
Hazard potential
Sector domain
Intensity or magnitude
Occurrence
/media/loftslag/Karlsdottir-Risk_analysis_IMO_SK.pdf
is on the northern North Atlantic and the Nordic Seas. With the southern
boundary at 47 N, the study domain covers Newfoundland, but excludes various marginal and
inland seas with significant independent storm activity, such as the Mediterranean and Adriatic
Seas, as well as the Black and Caspian Seas. The northern boundary at 80 N takes the domain
up to Fram Strait, including Svalbard, but excluding
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
Av. Ed.
Belin, 31400 Toulouse, France
Received: 21 March 2011 – Published in The Cryosphere Discuss.: 6 April 2011
Revised: 5 October 2011 – Accepted: 20 October 2011 – Published: 2 November 2011
Abstract. The Little Ice Age maximum extent of glaciers in
Iceland was reached about 1890 AD and most glaciers in the
country have retreated during the 20th century. A model for
the surface mass balance
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
emission scenario were even
greater, on average 5.1% units (Fig. 5), indicating that the GCMs are
a greater source of uncertainty than the choice of emission sce-
nario or RCM.
The flow regimes in different regions in Finland are demon-
strated with the five example hydrographs of the reference period
and of 2070–2099 (Fig. 8a–e, see Fig. 1c for locations). In northern
(Fig. 8a) and central (Fig. 8b/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
situations of strategic interaction.
4Contributions may depend on beliefs about others’ contributions in an environment with strategic uncer-
tainty; however, this effect does not pertain in an environment without strategic uncertainty.
5This limited choice was imposed in order to make the game as simple as possible and to yield clear theoret-
ical predictions depending on intrinsic preferences.
94/media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf
providing 11 minutes of warning time before the eruption.
The tremor signal emanating from Hekla travels outwards in a radial pattern, starting at stations
closest to Hekla and then traveling outwards towards the borders of Iceland. Figure 8 shows the
tremor amplitude plots for stations with a NE bearing from Hekla (Figure 8a) and a WSW
bearing from Hekla (Figure 8b). Figure 9 shows
/media/vedurstofan-utgafa-2021/VI_2021_008.pdf
of the three ice caps under consideration,
the horizontal displacement of the HRS and DMA DEMs
(40 m40 m spatial resolution) relative to the EMISAR
DEM (5 m5 m spatial resolution) was eliminated by
both maximizing the correlation and minimizing the
standard deviation of the elevation differences of ice-free
areas in the vicinity of the glaciers (gently sloping areas
within ca. 80800 m away
/media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf