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ORIGINAL ARTICLE
Climate change adaptation in European river basins
Patrick Huntjens • Claudia Pahl-Wostl •
John Grin
Received: 1 July 2008 / Accepted: 24 December 2009 / Published online: 2 February 2010
The Author(s) 2010. This article is published with open access at Springerlink.com
Abstract This paper contains an assessment and stan-
dardized comparative analysis of the current water man
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
the discharge in Skaftá and the
temperature of the flood water close to the glacier margin were measured. The dis-
charge from the subglacial lake during the jökulhlaup was calculated using a hypso-
metric curve for the subglacial lake, estimated from the form of the surface cauldron
after jökulhlaups. The maximum outflow from the lake during the jökulhlaup is esti-
mated as 123 m3 s 1 while
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
To distinguish between rain and snow, the volume is com-
pared to the water equivalent but the volume of snow is ten times larger.
Figure 1. How PWD22 determines the type of precipitation.
Using the information about the changes of the backscatter signal, water equivalent and temper-
ature the Vaisala Present Weather Detector can give information about the type of precipitation.
It is also used
/media/vedurstofan-utgafa-2019/VI_2019_009.pdf
scenario
development, with an example from Brazil
Kasper Kok *
Land Dynamics, Department of Environmental Sciences, Wageningen University, P.O. Box 47, 6700 AA Wageningen, The Netherlands
1. Introduction
The world is undergoing rapid changes while globalising
constantly, which gives the consideration of the future new
urgency and importance. Scenario development has emerged as a
key method when taking
/media/loftslag/Kok_JGEC658_2009.pdf