in an overall
cold bias, compared with station measurements. To test, whether this is due to the HARMONIE
model core or the external surface scheme, biases of 2-m temperature from SURFEX are com-
pared with biases of temperature projected from the lowest two model levels to 2 mAGL. It is
found that the negative temperature biases are due to shallow inversion layers near the ground,
which are introduced
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
; fax: +358 20 490 2590.
E-mail address: Noora.Veijalainen@ymparisto.fi (N. Veijalainen).
Journal of Hydrology 391 (2010) 333–350
Contents lists available at ScienceDirect
Journal of Hydrology
journal homepage: www.elsevier .com/ locate / jhydrol
Author's personal copy
narios from GCMs or RCMs, and with different emission scenarios
(e.g. Menzel et al., 2006; Minville et al., 2008; Prudhomme and Da
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
to highly
negative summer balances, but also lower bw than
the average for 1949–2006. Calculated change in
specific mass balance for a ±1°C change in air tem-
perature was ±0.55 m w.e., whereas a ±10 % in-
crease in precipitation represented a change of ±
0.20 m w.e. Model results further indicated that for
a 2°C warming, the ablation season will be extend-
ed by c. 30 days and that the period
/media/ces/GA_2009_91A_4_Andreassen.pdf
)
Use this model to identify policies that are likely to
succeed or that probe key uncertainties;
(2)
being to
(1) Work with stakeholders to develop a shared under-
standing of the system to be managed and the desirable
outcomes, by developing a system model that can be
used for policy screening;
Wal
as a
d
e social and political values in water resource
ment.
ters and Holling (1990) describe
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
surface velocity (Table 2 and com-
parison on profile DD’ in Fig. 6a), indicating that the model
captures the large-scale flow pattern of the glacier.
The 20th century glacier runoff anomalies, relative to a ref-
erence runoff computed at the start of the model simulations,
from the area that was ice-covered at LIAmax (234 km2) was
computed from the mass balance and precipitation fields
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
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