no authorisation is given to change data or any other information available from this web-site, unless the source and modification is stated clearly. (i.e., a description of data sourced from IMO and the subsequent changes made by others.)
The Icelandic Met Office's website does not collect personally identifiable data about users. Web traffic on en.vedur.is is measured by Google Analytics, Siteimprove
/about-imo/the-web/conditions
no authorisation is given to change data or any other information available from this web-site, unless the source and modification is stated clearly. (i.e., a description of data sourced from IMO and the subsequent changes made by others.)
The Icelandic Met Office's website does not collect personally identifiable data about users. Web traffic on en.vedur.is is measured by Google Analytics, Siteimprove
/about-imo/the-web/conditions/
of volcano-
tectonic structures are sets of parallel, northerly striking transcurrent faults that generate the largest
earthquakes in this zone, up to M 6.5. Their surface expressions are en echelon fracture arrays and
push-up structures. The sense of displacement is right-lateral. The distance between them varies from
0.5 to 5 km, and together they form a bookshelf-type fault system taking up the left
/media/norsem/norsem_palli.pdf
the day and can be checked anytime. A personal weather watch will send notifications when certain criteria are met, e.g. a forecast of temperature below zero at your chosen weather station.
An interactive weather map shows weather observations at any station in the country.
Get the weather app at Google Play Store or Apple App Store. Type VEDUR to find the app and install. Select language under
/about-imo/news/nr/2812
is situated in a seismically quiet intraplate setting in northern Europe. Intraplate
seismicity has been attributed to ridge-push from the North Mid-Atlantic Ridge, post-glacial rebound
stresses and to local gravitational potential energy differences associated with compositional
differences and crustal thickness variations.
Based on a subset of the most recent earthquake data (2000-2012
/media/norsem/norsem_korja.pdf
conditions
An interactive weather map shows weather observations at any station in the country.
Installation
Get the weather app at Google Play Store or Apple App Store. Type VEDUR or vedur to find the app and install. Select language under Settings (Stillingar), shown in the video below.
Video instructions
A video shows all the features of the weather app for those who want to familiarise
/about-imo/news/nr/3224
and explored. The list of earthquakes updates every five minutes. Click this link to run the model:
An interactive 3D model of the earthquakes in Bárðarbunga – preliminary version
However, this is a preliminary version; the model is still being developed. There are some browser issues, e.g. Google Chrome and Firefox run it, IE10 does not; other browsers have yet to be tested. In some instances
/earthquakes-and-volcanism/articles/nr/2971
and explored. The list of earthquakes updates every five minutes. Click this link to run the model:
An interactive 3D model of the earthquakes in Bárðarbunga – preliminary version
However, this is a preliminary version; the model is still being developed. There are some browser issues, e.g. Google Chrome and Firefox run it, IE10 does not; other browsers have yet to be tested. In some instances
/earthquakes-and-volcanism/articles/nr/2971/
is influenced by:
1. The individual’s characteristics (e.g., background
characteristics, attitudinal factors)
2. The attributes of the policy measure (e.g., push versus pull)
Steg & Schuitema (2007)
6
(2) Factors important for
acceptability cont.
• The multiattribute evaluation model describe factors
important for evaluations of structural changes to social
dilemmas – preference for status quo
/media/loftslag/Eriksson_2-Acceptability-of-policy.pdf
water infra-
structure projects begun now are large
enough to push hydroclimate beyond the
range of historical behaviors (19). Some
regions have little infrastructure to buffer the
impacts of change.
Stationarity cannot be revived. Even with
aggressive mitigation, continued warming is
very likely, given the residence time of
atmospheric CO2 and the thermal inertia of
the Earth system (4, 20
/media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf