The data are further interpolated onto a 1x1 grid
within WaSiM.
During the calibration of Sandá í Þistilfirði, snow melt was observed to start unreasonably
too early independently of parameterization, and most of the winter snow pack was melted
already in January leaving no snow to be melted during April as observed. This led to
suspicion about the quality of the simulated temperature data
/media/ces/2010_016.pdf
Adaptation in Finland
In Finland, adaptation policy development has taken place mainly through the preparation
process for the Finnish NAS in 2003, published in 2005 out of the recognition that adaptation
will be required irrespective of the success of mitigation measures (Marttila, Granholm et al.
2005). The preparation of the NAS was led by the Ministry of Agriculture and Forestry
/media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf
:
1) Recent advances in econometrics and economic geography have led to the reconsideration of the role of
space in socioeconomic studies, and the development of new models, which explicate, e.g. spatial
multipliers. This is a welcomed improvement in the study of climate change impacts and adaptation in the
city. However, such models require, to varying extents, the a priori conceptualisation
/media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
) focus on the importance of multiple frames or ambiguity among
stakeholders and decision makers in the environmental management process. These
approaches combined could be useful within the context of identification of uncertainty in
the IWRM process.
Recently, cooperation between ecologists and water managers has led to attempts to
integrate an ecosystem approach into IWRM. This approach
/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
and/or Herðubreiðartögl, all below magnitude 2.
18 September 2014 18:50 - from geoscientist on duty
Nearly 150 earthquakes have been recorded since midnight. About 45 of them occurred in Bárðarbunga, the largest a magnitude 5.3 at the northern rim of Bárðarbunga caldera at 14:22. The GPS station on Bárðarbunga showed a drop of 15 - 20 cm at the time of the earthquake. Two earthquakes occurred with magnitudes
/earthquakes-and-volcanism/articles/nr/3001
station on Bárðarbunga showed a drop of 15 - 20 cm at the time of the earthquake.
Two earthquakes occurred with magnitudes between 4 and 5 and four of magnitudes between
3 and 4. Over 50 earthquakes were recorded along the northern part of the dyke, all within
magnitude 2. About 30 earthquakes were recorded by Herðubreið and Herðubreiðartögl, all
with magnitudes below 2.
18 September 2014
/media/jar/Bardarbunga-2014_September-events.pdf
and/or Herðubreiðartögl, all below magnitude 2.
18 September 2014 18:50 - from geoscientist on duty
Nearly 150 earthquakes have been recorded since midnight. About 45 of them occurred in Bárðarbunga, the largest a magnitude 5.3 at the northern rim of Bárðarbunga caldera at 14:22. The GPS station on Bárðarbunga showed a drop of 15 - 20 cm at the time of the earthquake. Two earthquakes occurred with magnitudes
/earthquakes-and-volcanism/articles/nr/3001/