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the melt (e.g. Laumann and Reeh 1993;Braithwaite 1995). Surface energy balance mod-
els compute each of the relevant energy fluxes be-tween the atmosphere and the surface and require
additional meteorological measurements and ob-
servations, for example cloudiness and humidity.For studies of climate sensitivity to free-atmos-phere changes, data from stations outside the gla-
cier boundary layer
/media/ces/GA_2009_91A_4_Andreassen.pdf
....................................................................................... 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
environment and their rela-
tionship to regional climate changes has increased greatly since the
TAR. The quality of the data sets has also improved. There is a
notable lack of geographic balance in data and literature on ob-
served changes, with marked scarcity in developing countries.
{WGII SPM}
These studies have allowed a broader and more confident as-
sessment of the relationship between observed
/media/loftslag/IPPC-2007-ar4_syr.pdf
1998] and RCM output such
as incoming and outgoing, short- and long-wave radiation,
temperature, water vapor pressure, and wind speed:
ETref ¼
0:408D Rn Gð Þ þ g 900T þ 273 u2 es eað Þ
Dþ g 1þ 0:34u2ð Þ ð3Þ
where ETref is reference evapotranspiration (mm d1), Rn is
net radiation at the crop surface (MJ m2 d1), G is soil heat
flux density (MJ m2 d1), T is mean daily air temperature
at 2 m
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
of how climate change will
impact our countries” says Árni.A sustainable solution Powered entirely by Icelandic hydropower and geothermal energy sources
and taking advantage of the local tempered climate for keeping the
supercomputer components cool, the running costs and CO2 footprint
will be kept to a minimum, saving tonnes of CO2 in line with the
four nations' efforts towards reaching Net/about-imo/news/joining-forces-in-weather-forecasting-and-climate-research
(DGPS) equipment
in 2001. Continuous profiles, approximately 1 km apart,
were measured in the accumulation zone and a dense net-
work of point measurements were carried out in the abla-
tion zone. Digital Elevation Models (DEMs) of the surface
and bedrock were created from these data (Fig. 2; Björns-
son and Pálsson, 2004). The estimated errors are at most
1–5 m (bias less than 1 m) for the surface
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
for flood discharge analysis are located near the flood inundation
analysis sites.
The four sites for flood inundation analysis were selected from
areas where major flood damages have occurred and which are
listed as flood prone areas by Timonen et al. (2003). The national
flood hazard mapping with 20–1000 year floods, based on ob-
served and extrapolated flood discharges, was also carried out
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
of radiation are
added to a classic degree-day model. For infiltration, a methodology of Peschke, based on
the approach of Green and Ampt, was used. To calculate the fluxes within the unsaturated
soil zone, the Richards equation was used. The groundwater table was modelled in both the
unsaturated zone module and the groundwater module. The coupling between both modules
was done by a net/media/ces/2010_017.pdf
recorded at 5-13 km depth, but fewer than
yesterday.
GPS deformation: Measurements from around Eyjafjallajökull indicate no major net
discplaceaments, suggesting a stabilization of the surface deformation
since yesterday.
Other remarks: Grainsize analysis of samples taken of ash that fell on May 3rd at 64
km distance from the eruption site shows that about 5 % of the ash is
smaller
/media/jar/Eyjafjallajokull_status_2010-05-07_IES_IMO.pdf