Hydrological Sciences Journal, 53, 100-111.
Kriauciuniené, J., Meilutyté-Barauskiené, D., Rimkus, E., Kays, J., Vincevicius, A. (2008). Climate change impact on hydrological processes in Lithuanian Nemunas river basin. Baltica, Vol. 21 (1-2), pp. 1-61. Vilnius. ISSN 3067-3064.
Lawrence, D., Haddeland, I. (2010). Uncertainty in hydrological modelling of climate change impacts in four Norwegian
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temperature of the year was measured at Egilsstaðir in
the East on 3 June, 24.9°C, but the lowest minimum was -25.3°C in Svartárkot in
the north-eastern upland on 30 March.The absolute maximum in Reykjavík was 21.3°C, on 27 July. The absolute
minimum in Reykjavík was -10.3°C on 31 January. The year was the warmest on record in the north-western part of the
country. The large bold numbers show
/about-imo/news/the-weather-in-iceland-in-2016
Adaptation conference 29-31 August 2012 – Helsinki – Rantapuisto
Guidelines for rapporteurs
Please report the sessions assigned to you (see table below)
You can swap sessions with another rapporteur, if the concerned rapporteur explicitly affirmed
that swap and no other time or task conflicts occur (this is to be checked with the co-chair who
coordinates rapporteur slots – Adriaan
/media/loftslag/Guidelines2-for-rapporteurs.pdf
8
Stakeholder relevance of the CES project
Jenny Gode1 and Philip Thörn1
1IVL Swedish Environmental Research Institute,
P.O. Box 21060, SE-100 31 Stockholm, Sweden, e-mail: jenny.gode@ivl.se
A structured dialogue has been held with a Swedish stakeholder, Vattenfall. The objectives
have been to discuss stakeholder relevance of the CES project and methods for stakeholder
/media/ces/ces-oslo2010_proceedings.pdf
( 2007). Estimating the spatial distribution of precipitation in Iceland using a linear model of orographic precipitation. J. Hydrometeorol., 8(6), 1285-1306.
Gudmundsson, S., Bjornsson,H., Magnusson,E., Berthier, E., Palsson,F., Gudmundsson,M. T., Hognadottir, Th. & Dall, J. (2011). Response of Eyjafjallajokull, Torfajokull and Tindfjallajokull ice caps in Iceland to regional warming, deduced
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