-time and
detects signal characteristics similar to previously observed eruptions using a three-fold
detection procedure based on: 1) an amplitude threshold; 2) the signal-to-noise ratio; and 3) an
emergent ramp-like shape. Data from six Icelandic eruptions was used to assess and tune the
module, which can provide 10–15 minutes of warning for Hekla up to over two hours of
warning for some other
/media/vedurstofan-utgafa-2021/VI_2021_008.pdf
such as tornadoes,
hail, lightning and dust storms. There is no clear trend in the annual
numbers of tropical cyclones. {WGI 3.2, 3.8, 4.4, 5.3, SPM}
2
Causes of change
Topic 2 Causes of change
36
Causes of change
This Topic considers both natural and anthropogenic drivers of
climate change, including the chain from greenhouse gas (GHG)
emissions to atmospheric concentrations to radiative
/media/loftslag/IPPC-2007-ar4_syr.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
.............................................................................................. 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
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
than can be expected to originate from the cauldrons, three to four times the wa-
ter equivalent of the accumulation of snow over the watershed of the cauldrons. It has
been estimated that flow from the cauldrons, in addition to the jökulhlaups, could be
2–5 m3 s 1 at maximum (Vatnaskil, 2005). It is possible that part of the sulfate-rich
groundwater from the glacier comes from the cauldrons
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
...........................................................................................................8
2 Equipment inventory, age and health ...............................................................................9
2.1 Network health ...........................................................................................................9
2.2 Equipment inventory ................................................................................................10
2.3 Receivers
/media/vedurstofan/utgafa/skyrslur/2011/2011_005.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