maps for 1971-2000
Daily precipitation maps are available on request and further information on the making of the maps. IMO's contacts for this project are Philippe Crochet and Tómas Jóhannesson.
Reference:
Crochet, P., T. Jóhannesson, T. Jónsson, O. Sigurðsson, H. Björnsson, F. Pálsson and I. Barstad (2007): Estimating the spatial distribution of precipitation in Iceland using a linear model
/weather/articles/nr/1625
Projections
-50%
-48%-73%
-78%
-80%
+3%
Storglaciären Mårmaglaciären
Scandinavia
Comparison with all other glacier regions
Volume reduction and sea-level equivalent (SLE)
until 2100 for 19 glacier regions
Radic and Hock, submitted
Antarctica
Sub-Antarctic Islands
Greenland
New Zealand
South America II
South America I
Iceland
Arctic Canada
West Canada and West US
Alaska
High Mountain Asia
North
/media/ces/Hock_Regine_CES_2010rs.pdf
Neotectonics in Nordland; NEONOR 2
C. Lindholm, O. Olesen, I. Janutyte, S. Gradman, M. Keiding, H. Kierulf,
M. Ask, J. Dehls, Y. Maystrenko, F. Riis, L. Rise and other project partners
The Nordland shore region is known to be seismically active with deep local sediment basins on the
continental shelf that stretches some 200 km west of the coastline. The offshore areas west of Nordland
have
/media/norsem/norsem_lindholm.pdf
mover’s payoff, while mover 2’s
payoff is greater than or equal to the first mover’s payoff.
The payoff function is that of the basic public good game. The marginal return from the
public good is a ∈ [0,1], and each agent’s initial endowment is E. The payoff function Rik
of agent i as mover k, k = 1 for the first mover and k = 2 for the second mover, is defined
as follows:
Rik =E − xik + a (xik
/media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf
to improve our world," says Esri president Jack Dangermond. "Each year I look forward to being part of this ceremony. It is a tradition that means a great deal to Esri and to GIS professionals."
More information is available about the 2011 Special Achievement in GIS Award winners, including project information and photos. There, examples of IMO's work can be seen
/about-imo/news/nr/2241
and sustainable society. The main vision of the European Plate
Observing System (EPOS) is to address the three basic challenges in Earth Sciences: (i) unravelling the
Earth's deformational processes which are part of the Earth system evolution in time, (ii) understanding
the geo-hazards and their implications to society, and (iii) contributing to the safe and sustainable use
of geo-resources
/media/norsem/norsem_atakan_ip.pdf
/j.jenvman.2007.05.009
Huntjens P, Pahl-Wostl C, Grin J (2010) Climate change adaptation in European river basins. Reg. Environ. Change, 10, 263-284. DOI 10.1007/s10113-009-0108-
6
IPCC (2007) Climate Change 2007: Synthesis Report. Contribution of Working Groups I, II and III to the Fourth Assessment Report of the Intergovernmental Panel
on Climate Change. IPCC, Geneva, Switzerland, 104 pp
/media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf
1
Probability distributions of monthly-to-annual mean temperature and
precipitation in a changing climate (CES Climate Modelling and Scenarios
Deliverable D2.4, task I)
Jouni Räisänen
Department of Physics, P.O. Box 48, FI-00014 University of Helsinki, Finland
Email: jouni.raisanen@helsinki.fi
17 November 2009
AVAILABLE FROM:
http://www.atm.helsinki.fi/~jaraisan/CES_D2.4
/media/ces/CES_D2.4_task1.pdf