boundary flux between the unsaturated zone and the groundwater (Schulla
& Jasper, 2007).
Information on land use, soil type, elevation and other general properties of the watershed
are given in static distributed grids while a number of parameters describing specific
processes are adjusted to the properties of each watershed by comparison of modelled and
measured discharge series.
In this study
/media/ces/2010_017.pdf
by level of the analytical process
• Paradigm level: e.g. long term evolution in societal value
systems and prioritization structures
• scenario choices; delineation; (model type choice)
• Conceptual level: understanding of the causal structure
• Model (type) choice; model structure; data sources/needs
• Model level: sufficiently adequate representation of the causal
structure and orders
/media/loftslag/Perrels-CBA.pdf
and Surtsey would form a 3 cm thick deposit on Heimaey ....................... 36
Figure 15: Frequency of wind direction and wind speed ......................................................... 37
Figure 16: Probability of location of future vent opening based on the best fit line of the
identified previous vents
/media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf
conditions encountered by an aircraft in flight. This information is usually relayed by radio to the nearest ground station. At a minimum the PIREP must contain a header, aircraft location, time, flight level, aircraft type and one other field.
All significant weather encountered by an aircraft in flight, either to or from any Icelandic airport or airstrip, shall be reported to the Icelandic
/weather/aviation/pirep/
of the earthquake fault in Ölfus
30.5.2008
The map shows the location of the damaging earthquake that struck yesterday afternoon. Most movement took place along the fault shown in green.
The black arrows denote right-lateral, strike-slip faulting. The same type/about-imo/news/nr/1312
package.
From the recorded data we obtained nearly 120 FPS of the earthquakes and assigned them with the
quality factors. We grouped the earthquakes into several groups according to their geographical
locations, and investigated the obtained results in each group separately. The overall results in the study
area show the dominating normal type of faulting and the N-S
/media/norsem/norsem_janutyte.pdf
The first map shows cloud cover measurements at a few stations in Iceland, along with information about cloud type and lowest cloud altitude (see following diagram). This information can be useful in evaluating the quality of the forecast.
Cloud cover observations are made every three hours at a few stations in Iceland. The latest observation is shown
/weather/articles/nr/1219
of the glaciers at their maximum at the end of the Little Ice Age (about 1890) and also at the end of the 20th century. On the map surge-type glaciers are distinguished from non-surge-type glaciers with a darker green color. A symbol shows volcanic calderas which are located underneath the glaciers. Also shown are place-names of all of the glaciers that have been given names.
An explanatory
/about-imo/news/nr/2712
........................................ 34
Bergström, S. and Andréasson, J.
Swedish Guidelines for Design Floods for Dams in a Changing Climate ............................................................ 36
3
HYDROLOGICAL PROJECTIONS, GLACIERS AND ICE-SHEETS
Jóhannesson, T., Aðalgeirsdóttir, G., Ahlstrøm, A., Andreassen, L.M., Beldring, S., Björnsson, H., Crochet, P.,
Einarsson, B
/media/ces/ces-oslo2010_proceedings.pdf