49 results were found for 三分赛车pk10预算-【✔️访问㊙️700bet.net✔️】-e世博esball注册-AG捕鱼王新版app下载备用官网-(✔️网址sogou7.com✔️)-三分赛车pk10预算-三分赛车pk10预算-lpl外围在哪儿买登陆平台-【✔️网址㊙️700bet.net✔️】.
a systematic com-
parison of results to observed precipitation has been carried out. Un-
dercatchment of solid precipitation is dealt with by looking only at
days when precipitation is presumably liquid or by considering the
occurrence and non-occurrence of precipitation. Away from non-
resolved orography, the long term means (months, years) of observed
and simulated precipitation are often
/media/ces/Paper-Olafur-Rognvaldsson_92.pdf
with 20% and 2% for the HIRHAM experiments
using HadAM3H and with 30% and 7% for the ECHAM-
driven experiments for Middle Europe and Scandinavia,
respectively.
[18] RCM output is not available for the entire period
1961–2100 because transient RCM simulations are com-
putationally very demanding. Instead two 30-year time
slices are available; one representative for the climate in
the period 1961–1990
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
Journal of Environmental Management 88
Heid
, Øste
d
e
A broad range of tools are available for integrated water resource management (IWRM). In the EU research project NeWater, a
Human dependence on water leaves us vulnerable to
climate change, flood and drought hazards, and poverty
dynamic element of vulnerable groups and their relation-
ship to water resources, and to represent the decisions
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
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
Grin’s work on this article was part of the programme of the
Dutch Knowledge network on System Innovations (KSI).
P. Huntjens (&) C. Pahl-Wostl
Institute for Environmental Systems Research,
University of Osnabruck, Barbarastraße 12, Geb. 66,
49069 Osnabruck, Germany
e-mail: patrickhuntjens@yahoo.com
J. Grin
Amsterdam School for Social Science Research,
University of Amsterdam, Amsterdam
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
the average of the (wind speed) distribu-
tion is given by
m = AG(1+1=k) ; (2)
with gamma function, G, defined as usual. Wind power density, a measure of the energy flux
through an area perpendicular to the direction of motion, varies not only with the cube of wind
15
Figure 2. Annual modelled distributions (dashed lines) and corresponding Weibull fits
(solid lines) of wind speed at 50 mAGL, for two
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
the variations in the seasonal componentsof the mass balance;
– use the model to reconstruct the mass balanceprior to 1949;
– study the sensitivity of the model to differentmodel set ups and choices of parameters;
– and study the climate sensitivity of the glacierand implications of climate change on the massbalance.
SettingStorbreen (61°36' N, 8°8' E) is located in the Jotun-heimen mountain massif
/media/ces/GA_2009_91A_4_Andreassen.pdf