at Springerlink.com
Abstract We propose a generic framework to characterize climate change adaptation
uncertainty according to three dimensions: level, source and nature. Our framework is
different, and in this respect more comprehensive, than the present UN Intergovernmental
Panel on Climate Change (IPCC) approach and could be used to address concerns that the
IPCC approach is oversimplified. We have studied
/media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf
for Iceland were made. The CE
project used an ensemble of six GCMs and RCMs from the PRUDENCE project for four different
emissions scenarios (B1, B2, A2, and A1FI) developed by the Intergovernmental Panel on Climate
Change (IPCC). The GCMs used by the CE project showed more warming during winter than
summer. During winter, the median projected warming from 1961–90 to 2070–99 ranged from
3–6 K, and from 2
/media/ces/2010_005_.pdf
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/media/ces/2010_017.pdf
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/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
International Panel on Climate Change (IPCC)
UN Framework Convention on Climate Change
NOAA Climate Program Office
NASA Climate and Radiation Branch
/climatology/iceland/climate-report
International Panel on Climate Change (IPCC)
UN Framework Convention on Climate Change
NOAA Climate Program Office
NASA Climate and Radiation Branch
/climatology/iceland/climate-report/
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
due to weather conditions or malfunction in the power production
equipment. For stations that only have solar panel power, this occurs mainly during high
winter. The stations therefore go on stand-by until sufficient power is available. This fact
can affect the completeness of the time-series gathered from these stations. It is therefore
recommended that the completeness of data series
/media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf
such as
irrigation, CO2 effects on transpiration, and land use changes affect the water balance to a
lesser extent.
Citation: van Roosmalen, L., T. O. Sonnenborg, and K. H. Jensen (2009), Impact of climate and land use change on the hydrology of
a large-scale agricultural catchment, Water Resour. Res., 45, W00A15, doi:10.1029/2007WR006760.
1. Introduction
[2] The most recent Intergovernmental Panel/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf