23 results were found for 太阳3娱乐官方地址-太阳3娱乐官方地址-【✔️输入㊙️bet25.net✔️】-太阳3娱乐官方地址-太阳3娱乐官方地址-【✔️访问㊙️360bet.net✔️】-太阳3娱乐官方地址-太阳3娱乐官方地址-太阳3娱乐官方地址-(✔️访问sogou7.com✔️).
....................................................................................... 10
3 September 2012 .................................................................................. 12
3 Radiation fluxes at the surface ....................................................................... 16
4 Heat fluxes at the surface .............................................................................. 21
5 Net energy
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf
, Veðurstofu Íslands
Contents
1 Introduction ................................................................................................ 7
2 Model setup and data ................................................................................... 7
3 Model terrain and surface type ...................................................................... 9
4 Impact of initial conditions in blending
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
either in exploiting
or protecting the resource. Stakeholders include the fol-
lowing categories: (1) competent water resource authority
(typically the water manager, cf. above); (2) interest
groups; and (3) general public.
1544 J.C. Refsgaard et al. / Environmental Modellin
The modelling process may, according to the HarmoniQuA
project (Refsgaard et al., 2005a; Scholten et al., 2007, http
/media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
economic growth and over-
all emissions. {WGIII 3.2, TS.3, SPM}
Aerosols have a net cooling effect and the representation of
aerosol and aerosol precursor emissions, including sulphur diox-
ide, black carbon and organic carbon, has improved in the post-
SRES scenarios. Generally, these emissions are projected to be lower
than reported in SRES. {WGIII 3.2, TS.3, SPM}
Available studies indicate
/media/loftslag/IPPC-2007-ar4_syr.pdf
networks for
t
i Christiansen Barlebo
r Voldgade 10, DK-1350 Copenhagen K, Denmark
form 3 May 2007; accepted 11 May 2007
29 June 2007
www.elsevier.com/locate/jenvman
Mak
manage
ARTICLE IN PRESS
brought together to find a solution that is adequate from
multiple perspectives. This, not only requires coping with
various sources and types of uncertainty, but also with the
ambiguity produced
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
bursts of
seismic tremor (1–3 Hz), and later becoming
periodic with energy between 2 and 8 Hz. After
18 October, seismicity increased to three events
per day (Figure 2b). Synchronous with this
increase, the ISGPS station SKRO (Figure 1b)
moved 9 mm westward over the following eight
days, and returned to its original position on 1
November (Figure 2c), suggesting subsurface
magma movement
/media/jar/myndsafn/2005EO260001.pdf
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
; 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