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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/
of seismicity with respect to longitudes.
NATIONAL COMMISSIONER OF THE ICELANDIC POLICE
DEPARTMENT OF CIVIL PROTECTION AND EMERGENCY MANAGEMENT
Graph a Graph b
Figure 7 Graph a) shows a time series for the GPS station in Vonarskad (VONC), the station is labelled with a black box
on the earthquake map above. The time series shows a change in the location of the station to the north (top/media/jar/Factsheet_Bardarbunga_20150130.pdf
in Figure 2). The
well screen is located 5.65 m below ground surface at
location A and 25.5 m below ground surface at location
B. Generally the model captures the dynamics in the time
series well, even though the mean simulated and observed
values may differ considerably. Therefore this study focuses
on spatially averaged changes when comparing one simu-
lation to the other and less on the absolute
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
Grímsvötn volcano
Status Report: 16:00 GMT, 2 November 2010
Icelandic Meteorological Office and Institute of Earth Sciences, University of Iceland
Compiled by: Thorunn Skaftadottir, Egill Axelsson, Rikke Pedersen,
Gunnar B. Gudmundsson and Matthew J. Roberts.
Based on: IMO seismic monitoring; IES-IMO GPS monitoring; IMO
hydrological data.
Meltwater: Water continues to drain from
/media/vatnafar/flod/Grimsvotn_status_2010-11-02_IES_IMO.pdf
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
coefficients are much more variable. A distinct maximum with a � 2
occurs along the western coast of Norway in winter and to a lesser extent in autumn. The
constant offsets b show some tendency to anticorrelation with a, particularly for temperature
6 A slight systematic tendency for the coefficients to exceed one can be seen, particularly
/media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf
of lifecycle costing approach is allowed in the evaluation
of how to prioritize maintenance needs.
The maintenance task interacts with operational tasks (like snow clearing) and strategic tasks
(road planning). Budget pressures in one task group may lead to cost rises in another. For
example, some asphalt types may require more often salting against slippery conditions than
other ones
/media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf
was chosen because after 1980 sea ice is fully initiated in RCAO
and after 2006 the records from the weather-stations end. (The stations actually continue to
4
Figure 2: mass balance profiles calculated using RCAO (Plot a) and
HIRHAM4 (Plot b) for model input.
measure, but in the short time available for the Paakitsoq mass balance project we did not
look for more data.) The reference period
/media/ces/ces_geus_paakitsoq_full_report.pdf