to increase in Finland by 13–26% by the 2080s (Ruosteenoja
and Jylhä, 2007) and extreme precipitations are expected to in-
crease (Beniston et al., 2007). On the other hand, temperature in-
creases of 2–6 C by the end of the century are estimated to
decrease the snow accumulation by 40–70% by the same period
(Vehviläinen and Huttunen, 1997; Beldring et al., 2006; Ruosteeno-
ja and Jylhä, 2007
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
Forms of Participatory Modelling and its Potential for
Widespread Adoption in the Water Sector
Matt Q1Hare
Durango 330, Depto 2, Roma Norte, Cuauhtemoc, Mexico D.F. 06700, Mexico
ABSTRACT
This article serves as a support for those interested in learning more about participatory
modelling and its potential for widespread adoption by resource managers. The rst part
introduces the reader to four
/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
than can be expected to originate from the cauldrons, three to four times the wa-
ter equivalent of the accumulation of snow over the watershed of the cauldrons. It has
been estimated that flow from the cauldrons, in addition to the jökulhlaups, could be
2–5 m3 s 1 at maximum (Vatnaskil, 2005). It is possible that part of the sulfate-rich
groundwater from the glacier comes from the cauldrons
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
Conference on Future Climate
and Renewable Energy:
Impacts, Risks and Adaptation
31 May - 2 June 2010
Soria Moria Hotel and Conference Center, Oslo, Norway
Conference proceedings
1
Conference proceedings
Future Climate and Renewable Energy: Impacts, Risks and Adaptation
31 May – 2 June 2010
Soria Moria Hotel and Conference Center, Oslo Norway
Published by: Norwegian Water
/media/ces/ces-oslo2010_proceedings.pdf