: 115 km towards SW and 55 km towards NNE from Bárðarbunga
Trend: Veidivötn fissure swarm NE-SW, Dyngjuháls fissure swarm NNE-SSW
Ice cover: Partial
Type of activity: Lava effusion, explosive phreatomagmatic
Magma type: Basalt
Eruption characteristics:
Type of products: Airborne tephra, lava flows, water transported tephra
VEI Max: VEI 5-6; most freq: VEI 1-2
Bulk volume
/media/jar/Bardarbunga_kafli20140825.pdf
.............................................................................................. 45
5.3 Present weather ..................................................................................... 45
Appendix ......................................................................................................... 47
5
List of Figures
1 How PWD22 determines the type of precipitation. ........................................ 11
2 Number of records as a function of the height
/media/vedurstofan-utgafa-2019/VI_2019_009.pdf
Fault plane solutions of the earthquakes in Nordland, Norway
Ilma Janutyte(1), Jan Michalek(2), Conrad Lindholm(1), and Lars Ottemoller(2)
(1) NORSAR, Kjeller, Norway, (2) University of Bergen, Bergen, Norway
This study is a part of the ongoing NEONOR2 project which is carried out in Nordland, norther
Norway. This work aims to define the fault plane solutions (FPS) of the earthquakes
/media/norsem/norsem_janutyte.pdf
Assessment Re-
port (AR4).
Topic 1 summarises observed changes in climate and their ef-
fects on natural and human systems, regardless of their causes, while
Topic 2 assesses the causes of the observed changes. Topic 3 pre-
sents projections of future climate change and related impacts un-
der different scenarios.
Topic 4 discusses adaptation and mitigation options over the
next few decades
/media/loftslag/IPPC-2007-ar4_syr.pdf
countries in
hydrological climate change studies, and in Scandinavia HBV is
the most commonly used model type (Vehviläinen and Huttunen,
Table 2
Climate scenarios used in the study (Finnish Meteorological Institute, ENSEMBLES data archive) and their projected annual changes in temperature and precipitation in Finland by
2070–2099 compared with the reference period 1971–2000. The greatest
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
These
working hypotheses have been further developed into a
methodology for evaluating the level of Adaptive and
Integrated Water Management, which resulted in an ana-
lytical framework for assessing regime characteristics,
consisting of nine different dimensions of variables:
1. Agency
2. Awareness Raising & Education
3. Type of governance
4. Cooperation structures
5. Policy development
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
to be
estimated based on return periods for accumulated precipitation over a fixed timescale,
which is typically 24 hours.
10. Precipitation return periods need to be translated into engineering recommendations
suitable to the type of infrastructure and activity in question.
From the above list, this report addresses points 1, 2, 3, 4 and 7. Point 9 is considered but not
addressed completely
/media/vedurstofan-utgafa-2020/VI_2020_008.pdf
cover.
In Iceland and other countries located at around the same latitude and further north, low clouds are defined as clouds located up to 2 km in altitude and middle clouds from 2 km up to 4 km in altitude. A third cloud type, not shown on a specific map (however, the information appears on the map for total cloud cover), is high clouds which can reach from 3 km up to 8 km in altitude.
Main
/weather/articles/nr/1219