6University of Washington,
Seattle, WA 98195, USA. 7NOAA Geophysical Fluid
Dynamics Laboratory, Princeton, NJ 08540, USA.
*Author for correspondence. E-mail: cmilly@usgs.gov.
An uncertain future challenges water planners.
Published by AAAS
on July 12, 201
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” (Poster) at at ESF-COST High Level Research Conference “Extreme Environmental Events” in Cambridge, 13.-17. December 2010.
Jokinen, P. Several interviews especially related to severe weather, extreme heat and climate change for radio (~10 interviews), TV (one interview) and daily press (dozens) in late July and beginning of August.
Jylhä, K. Four interviews by TV channels in Septemer and December
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model setup are typically too large by up to an order of magnitude.
This, combined with strong forcing at the model boundaries, results in a systematic spatial bias in
low-level wind speed, with too strong winds in coastal regions, and too weak winds in the interior.
Figure 5 shows a comparison of average wind speed at 10 mAGL between the WRF model and
station measurements. Model data is interpolated
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scenario, precipitation increased by 10–15% from 1961–90 to
2070–99, and by 5–10% for the lower emitting scenarios (corresponding to approximately 0.5–1%
per decade).
The CE project also examined RCM results for Iceland based on the HIRHAM model (Haugen and
Iversen, 2006). These results showed enhanced warming over the interior of Iceland compared with
the coastal zone, and a tendency for enhanced
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2610 BIRI NO +60:57:10 +10:35:49 190 P
2611 ABJORSBRATEN NO +60:55:05 +09:17:25 639 TP
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2613 ESPEDALEN NO +61:25:00 +09:32:04 752 P
2614 LUNNER NO +60:17:39 +10:34:49
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