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
version of the manuscript.
References
Allen, R. M., G. Nolet, W. J. Morgan, K. Vogfjörd, M. Nettles, G. Ekström, B. H.
Bergsson, P. Erlendsson, G. Goulger, S. Jakobsdottir, B. Julian, M. Pritchard, S.
Ragnarsson, and R. Stefansson (2002). Plume driven plumbing and crustal formation in
Iceland, J. Geophys. Res., 107 (B8) 101029/2001JB000584.
Ágústsson, K., and Ó. G. Flóvenz (2005). The Thickness
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf
). Locations of the weather sta-
tions, used to reconstruct the temperature and precipitation records,
are shown with letters: Reykjavík (R), Fagurhólmýri (F), Hæll (H),
Stykkishólmur (S), Teigarhorn (T), Vestamannaeyjar (V), Akureyri
(A) and Hólar in Hornafjörður (HH). (B) The surface topography of
Vatnajökull ice cap. Dots show the sites of mass balance and veloc-
ity measurements, blue dots show
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
hraðamælingar á Langjökli jökulárið 2006-2007. Report in Icelandic. Institute of
Earth Sciences, University of Iceland. RH-22-2007.
Toutin, Th. 2006. Generation of DSMs from SPOT5-HRS and across-track HRG stereo data using spatiotrianglulation and autocalibration. ISPRS
Journal of Photogrammetry and Remote Sensing, 60(3), 170-181.
Zwally, H. J., B. E. Schutz, W. Abdalati, J. Abshire, C. Bentley, A. Brenner
/media/ces/glacier_mass_balance_poster.pdf
activity in Iceland 2015-2016 and testing
of
near real time automatic relative locations
Gunnar B. Guðmundsson and the Natural Hazards monitoring
team
09:20 – 09:40 24/7 monitoring of natural hazards at the
Icelandic Meteorological Office
Kristín Jónsdóttir and the Natural Hazards monitoring team 09:40
– 10:00
/norsem/norsem2016/program/wednesday
was derived from
observations in the area of Swiss Camp (h is the surface elevation in m a.s.l):
τcl = 1.0 − 0.78n
2 exp(−0.00085h) (3)
3.2 Validation Procedure
Implemented in the mass balance model is the comparison of the RCM-data (= the model
input) to observations from weather stations on the ground. The observations are compared
to the values of the RCM grid-cells they are located in. Before
/media/ces/ces_geus_paakitsoq_full_report.pdf
@vedur.is),
P. Crochet, Th. Thorsteinsson, O. Sigurðsson, B. Einarsson
Institute of Earth Science, University of Iceland and DMI
H. Björnsson, S. Guðmundsson, F. Pálsson, G. Aðalgeirsdóttir
Section for Glaciers, Snow and Ice, NVE
L. M. Andreassen, K. Melvold, H. Elvehøy
Uppsala University and Geophys. Inst., University of Alaska
R. Hock, V. Radic
Geocenter Copenhagen, GEUS
A. Ahlstrøm, H/media/ces/ces_flyer_glacierssnowandice.pdf
of climate change on the routine and periodic maintenance of roads. Helsinki
2009. Finnish Road Administration, Central Administration. Finnra reports 8/2009, 66 p. +
app. 8 p. ISSN 1459-1553, ISBN 978-952-221-172-9, TIEH 3201122-v. (in Finnish, abstract in English)
[5] Salanne, i., Byring, B., Valli, R., Tikkanen, R., Peltonen, P., Haapala, J., Jylhä, K., Tolonen-Kivimäki, O.,
and Tuomenvirta, H/media/loftslag/CASE_B__Heikki_Tuomenvirta_(FMI)_Introduction.pdf
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/media/loftslag/Group-1_Scenarios-for-AWM.pdf