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/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
NATIONAL COMMISSIONER OF THE ICELANDIC POLICE
DEPARTMENT OF CIVIL PROTECTION AND EMERGENCY MANAGEMENT
Press release
Date: 16.03.2015 Time: 10:00 Regarding: Reduction of the access controlled area north of Vatnajökull.
Corrected title on map.
The Police District Commissioners in North Eastern, Eastern, Southern Iceland, and the National Commissioner of the
Icelandic Police have decided
/media/jar/Access_conrolled_area_20150316.pdf
NATIONAL COMMISSIONER OF THE ICELANDIC POLICE
DEPARTMENT OF CIVIL PROTECTION AND EMERGENCY MANAGEMENT
Press release
Date: 13.02.2015 Time: 11:45 Regarding: The access controlled area north of Vatnajökull
The National Commissioner of the Icelandic Police and Police Districts Commissioners in North East, East and Southern
Iceland have decided (with reference to law on civil protection nr
/media/jar/Access_conrolled_area_20150213.pdf
ice volume stored in the glaciers, and preferably
also the progressive lowering of the ice surface and the reduction in glaciated area that are
associated with a reduction in ice volume. The current versions of the Swiss WaSiM and the
Norwegian HBV models effectively assume an inexhaustible reservoir of ice with an unchanged
altitude distribution, which may lead to an unrealistic contribution
/media/ces/ces-glacier-scaling-memo2009-01.pdf
Seismicity of the Nordland area, Norway
Jan Michalek, Lars Ottemoeller, Berit Marie Storheim, Marte Louise Strømme
University of Bergen, Norway
The Nordland area (65-70N; 8-18E) is tectonically active part of Norway. Enhanced seismicity may
reflect on off-shore subsidence combined with the uplift of landmasses usually attributed to glacial
isostatic adjustment (related
/media/norsem/norsem_michalek.pdf
in the morning of July 7th. The landslide crossed the river Hítará, damming
the river and causing a lake to form above the debris tongue. The water found a
new channel the next day into Tálmi, a riverbed that reconnects with Hítará a
few km farther downstream.The landslide was detected by a seismograph at 05:17 in the morning of July 7th. A fox hunter in the area heard a landslide at around 23
/about-imo/news/a-large-landslide-falls-in-hitardalur-valley
in the morning of July 7th. The landslide crossed the river Hítará, damming
the river and causing a lake to form above the debris tongue. The water found a
new channel the next day into Tálmi, a riverbed that reconnects with Hítará a
few km farther downstream.The landslide was detected by a seismograph at 05:17 in the morning of July 7th. A fox hunter in the area heard a landslide at around 23
/about-imo/news/a-large-landslide-falls-in-hitardalur-valley/
Observations - Reykjavik area - Other stations | Observations | Icelandic Meteorological office
Other stations |
Other areas
Observations - Reykjavik area - Other stations
Kópavogur - Fossvogsdalur | Reykjavík Háahlíð | Reykjavíkurflugvöllur
Mon 1.05 13 GMT
Kópavogur - Fossvogsdalur
6.2° E 4
Max wind : 4
/m/observations/areas
in the study area
both onshore and offshore. The improved station coverage in Nordland with 26 temporary seismic
stations in addition to the permanent deployments in Norway and Sweden enables to achieve this task
with higher precision compared to the previous studies. To obtain the FPS we used three different
programs: FOCMEC, HASH and FPFIT, which are implemented into the SEISAN program
/media/norsem/norsem_janutyte.pdf