Past changes in climate and
hydrology
Anders Moberg
Department of Physical Geography and Quaternary Geology
Stockholm University
Conference on Future Climate and Renewable Energy:
Impacts, Risks and Adaptation
Oslo, 31 May 2010
http://data.giss.nasa.gov/gistemp/
This year so far (Jan – Apr) ...
Temperature anomaly (°C) from 1951-80 mean
http://www.metoffice.gov.uk/climatechange/science
/media/ces/Moberg_Anders_CES_2010.pdf
by groundwater base flow.
2.2. Geology and Hydrogeology
[13] The main ice border of the Weichselian glaciation
was located at the Jutland Ridge, hence the shallow geology
in Western Jutland is dominated by glacial outwash sand
and gravel originating from the glaciers’ meltdown. Isolated
islands of Saalian sandy till are found between the outwash
plains (Figure 2). The thickness of the Quaternary/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf