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in other words, why should
participation be undertaken?
2. How can “good” or “effective” participation
be carried out and evaluated?
In addition, concepts and methods of stakeholder
analysis in natural resources management (Grimble
and Wellard 1997), as well as in public policy
analysis (Bryson et al. 2002), have been discussed
in detail to enable planners and policy makers to
better understand
/media/loftslag/vonKorff_etal-2010.pdf
important roles in the development of early
adaptation commitments, something that has been formalised for instance in an accord with
central level on Hampshire developing good practice examples on adaptation. Due to its
2 The new UK government from 2010 has removed the indicator system, making it less clear how this national-
local linkage
/media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf
• Openness of natural systems
• Duration, rhythm, and reversibility of changes (hysteresis).
Another example is the lack of confidence in predicting key economic and social variables.
Last but not least, uncertainties arise as a result of heterogeneous knowledge frames held by
multiple stakeholders. A good illustration is the fierce debate as to whether climate change is
taking place
/media/loftslag/Group5-Draft_report.pdf
of the data and the state
of the instruments that are still running is in many cases not known. The Reykjavík series from the
old harbour is the only one known to be of good quality (not only for some periods) (ibid.), even
though more frequent calibrations would have been needed there too and it is unclear how it is best to
calibrate the instrument since 1994 (Tryggvason, 2017). Proposals of a new sea
/media/vedurstofan-utgafa-2020/VI_2020_005.pdf
for temperature and lower for precipitation. Given
attention to the extremes, a more ambitious strategy for ensemble climate simulations is needed in
order to better address the problem of natural climate variability and how it may be affected by a
global climate change. Changes in the distribution of climatic events are as interesting as changes in
the mean when the impacts of climate change
/media/ces/CES_D2.4_VMGO.pdf
The perturbations DV and DA are defined as
differences with respect to a convenient choice of a reference glacier geometry which does not
need to correspond to a steady state.
The runoff contribution due to ice volume changes is given by the term d(DV )=dt on the left
hand side of Equation (3). The first term on the right hand side, B0, corresponds to the climate
forcing and is calculated without
/media/ces/ces-glacier-scaling-memo2009-01.pdf
to the surface, how long time that takes but it can take from minutes to hours. Because of interaction between magma and water the eruption become explosive and produces a volcanic plume that reaches commonly 5-12 km a.s.l. while the volcanic plume/cloud is transported by the wind, it spreads tephra over Vatnajökull ice cap and only a minor fraction outside the ice cap. In phreatomagmatic eruptions several
/volcanoes/grimsvotn-activity/faq/
)
– www.seeconsult.org
• UN–Water (water-related adaptation) (08-10)
• Participatory & adaptive water resources
management (99-onwards)
• Knowledge
– the enormous breadth of participatory methods
– participatory process design principles
• Understanding
– How to select methods for participatory processes
– The traps that can lead to participation being an
enormous waste of resources
• Skills
– How to do cognitive
/media/loftslag/Hare_1_PartINONAM.pdf
a year, or its variations with the season. The maps are available in small and large domain.
The numbers reported in brackets on the large domain map correspond to the number of times that some UST stations (marked with grey dots) measured a concentration higher than the threshold the map is referring to. The numbers refer to hourly averaged concentration of SO2.
At a specific location
/pollution-and-radiation/volcanic-gas/hazard-zoning/