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A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö
A
A: Icelandic abbreviation of East (compass direction, easterly, eastern).
ANA: Icelandic abbreviation of Eastnorthesast (compass direction).
ASA: Icelandic
/weather/articles/nr/1208/
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
a systematic com-
parison of results to observed precipitation has been carried out. Un-
dercatchment of solid precipitation is dealt with by looking only at
days when precipitation is presumably liquid or by considering the
occurrence and non-occurrence of precipitation. Away from non-
resolved orography, the long term means (months, years) of observed
and simulated precipitation are often
/media/ces/Paper-Olafur-Rognvaldsson_92.pdf
which are significantly lower com-
pared with similar beginning and end years. Consequently, for the 2004–50 period, the average
RCM warming rates of 0.29 K per decade over the ocean, and 0.35 K per decade over the land are
somewhat larger than for the reduced IPCC ensemble mean.
Additionally, the tabulated values of SAT differences between the 1961–90 control period and
either the 2021–50
/media/ces/2010_005_.pdf
to use the available new estimates
Mw(v) to build a PGA relationship that would give very similar results as model A. Due to the
more complicated relationship between Ci and Mw(v) in the acceleration case, a second order
polynomial was chosen as the functional form of h and thus through the least-squares method
we estimated the parameters b, c and d according to:
Ci = d·Mw2(v) + b·Mw(v) + c
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf
the volcanic
plume due to their size and weight fall close to the volcano and constitute the
proximal deposit. Smaller particles can reach higher altitudes and persist in the
atmosphere for days and weeks and be advected far away by the wind. This
fraction of the pyroclastic material can possibly generate a distal deposit
very thin and covering wide areas.Term Size Ballistic d > 64 mm Lapilli 2 mm < d/volcanoes/volcanic-hazards/volcanic-emissions/
The recent Bothnian Bay M4.1 earthquake: where, how and why?
B. Lund1, M. Uski2, H. Shomali1, D. Buhcheva1, S. Amini1, J. Kortström2
1Dep. of Earth Sciences, Uppsala University, Sweden
2Institute of Seismology, Dep. of Geosciences and Geography, University of Helsinki, Finland
On 19 March 2016 a magnitude 4.1 earthquake occurred in the Bothnian Bay, between northern
Sweden
/media/norsem/norsem_lund.pdf
example
can be given by the low cost still flood risk adaptation by implementing early warning system. But
there is one more suggestion dfor stakeholders to restrict infrastructure in the cities of Horsens.
Fiva PhD Courses : Adaptive management in relation to climate change (august 22 2011 - august 26 2011)
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/media/loftslag/Group-1_Scenarios-for-AWM.pdf
Tengö, D. Timmer,
and M. Zurek. 2007. Linking futures across scales:
a dialog on multiscale scenarios. Ecology and
Society 12(1): 17. [online] URL: http://www.ecolog
yandsociety.org/vol12/iss1/art17/.
Borgatti, S. P., and P. C. Foster. 2003. The network
paradigm in organizational research: a review and
typology. Journal of Management 29(6):991-1013.
Brenner, N. 2001. The limits to scale
/media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf