) noted that Iceland had a maritime
climate that was much milder than its position on the globe might suggest. In
data from 1981–2010, Iceland annual average temperatures ranged from 6°C at the
south coast to 3°C at the north coast, with a substantially colder highland
interior. In comparison with the latitudinal average for the same period, the
coastal temperatures in Iceland are 8–10°C warmer
/climatology/iceland/climate-report
) noted that Iceland had a maritime
climate that was much milder than its position on the globe might suggest. In
data from 1981–2010, Iceland annual average temperatures ranged from 6°C at the
south coast to 3°C at the north coast, with a substantially colder highland
interior. In comparison with the latitudinal average for the same period, the
coastal temperatures in Iceland are 8–10°C warmer
/climatology/iceland/climate-report/
Energy source
- Catchment area
- Collection area
- Wind
- Biomass
- etc.
2. Power Plant
- Technique
- Maintenance
- Personnel
- Organisation
- etc.
902/07/2010
Tools for risk/opportunity identification
very likely
2.1 - M o re rainfall:
annual runo ff w ill
inc rease 0 -8 %
Sc en ario 2. inc reased p re cip itation
1.2 - …
very likelyinc rease turbine
capa city
increased
electrica l
resis
/media/ces/Keranen_Jaana_CES_2010.pdf
of radiation are
added to a classic degree-day model. For infiltration, a methodology of Peschke, based on
the approach of Green and Ampt, was used. To calculate the fluxes within the unsaturated
soil zone, the Richards equation was used. The groundwater table was modelled in both the
unsaturated zone module and the groundwater module. The coupling between both modules
was done by a net
/media/ces/2010_017.pdf
in Figure 8a are colored
green, while the three to the NE plotted in Figure 8b are colored yellow.
Table 2. Table of the visually picked arrival times of the Hekla 2000 eruption tremor to
stations WSW of the volcano (hau, sau, kri, grv) and NE of the volcano (skr, ren, gil). Tremor
velocities are with respect to the previous station.
Bearing
from
Hekla
Station
Name
Distance
from
/media/vedurstofan-utgafa-2021/VI_2021_008.pdf
6University of Washington,
Seattle, WA 98195, USA. 7NOAA Geophysical Fluid
Dynamics Laboratory, Princeton, NJ 08540, USA.
*Author for correspondence. E-mail: cmilly@usgs.gov.
An uncertain future challenges water planners.
Published by AAAS
on July 12, 201
1
www.sciencemag.or
g
Downloaded from
1 FEBRUARY 2008 VOL 319 SCIENCE www.sciencemag.org574
POLICYFORUM
combined with opera-
tions
/media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf
” (Poster) at at ESF-COST High Level Research Conference “Extreme Environmental Events” in Cambridge, 13.-17. December 2010.
Jokinen, P. Several interviews especially related to severe weather, extreme heat and climate change for radio (~10 interviews), TV (one interview) and daily press (dozens) in late July and beginning of August.
Jylhä, K. Four interviews by TV channels in Septemer and December
/ces/publications/nr/1680
national and local power companies 40% and finally Reykjavik City and others 17%.
In spite of the increased importance of this resource, the network system has diminished by 30% since 2008, i.e. fewer gauging and monitoring stations are operating today.
Summary
The climate and hydrology of Iceland are highly variable due to natural conditions.
Significant changes in these factors over the last 15
/about-imo/news/nr/2910
Participatory
methods and processes
for adaptive management
Dr Matt Hare
Independent Consultant, Mexico City
Adaptive and participatory water management
Matt Hare, hare@gmx.de 2011 – Summer School
About myself ...
• Bachelor in artificial intelligence (88-92)
• PhD environmental modelling in knowledge
and data-poor domains (95-99)
• Co-founder of Seeconsult GmbH (03-onwards
/media/loftslag/Hare_1_PartINONAM.pdf
groups, while
decentralisation may further result in a larger role for city networks or voluntary local level
declarations in decision-making (Rhodes 2000). Given that some processes have moved up to
the international level (or in Europe, to the EU level), network governance may also allow
some actors to “jump scale” (Gupta 2008, Princen 2007) by drawing on or even lobbying
processes
/media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf