...................................... 12
Kriauciuniene, J., Reihan, A., Kolcova, T., Meilutyte-Barauskiene, D. and Lizuma, L.
Regional temperature, precipitation and runoff series in the Baltic countries ...................................................... 14
Fleig, A.K., Tallaksen, L.M., Hisdal, H. and Hannah, D.M.
Regional hydrological drought in north-western Europe and associated weather types
/media/ces/ces-oslo2010_proceedings.pdf
Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009
ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost
operating manage- ment develop- poned-, of land grants ons European tax over- level
costs ment ment comprehen- build- and com- Regional De- heads
1991- 1991- sive- and ings pensation
/media/loftslag/Traffc-maintenance_expenditures.pdf
and G17. .................. 52
Figure 3.23. Seismicity and mapped faults in box J, near to the village of Hella. .............. 53
Figure 3.24. Seismicity and mapped faults in boxes K, near to Hraungerði in Flói
district and L, Skeið district. ............................................................................ 54
Figure 3.25. Seismicity and mapped faults in the easternmost box M, Land
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
and a river close to the site and a lake nearby. Elevation is 65 m above sea level, distance from the sea is 26 km and distance to towns of about 1000 inhabitants is about 15 km. This is an ideal inland background station at 64oN 21oW.
Since 1980, daily sampling has been done at Írafoss, monitoring sulphur concentrations and related substances. In fact, daily sampling was done at Rjúpnahæð
/pollution-and-radiation/pollution/
Columbia
University Press.
O'Neill, R.V., D. DeAngelis, J. Waide and T. F. H. Allen. 1986. A hierarchical
concept of ecosystems. Princeton University Press.
Log time
(years)
Log space
(meters)
Leaf
Crown
days
Tree Stand
Forest
Branch
Landscape
months
year
century
decade
cm m 100m 100km
Examples of functional scales
Log time
(years
/media/loftslag/Kok_1-scenarios-lecture-1.pdf
by the snowpack, per hour and
unit area (energy flux), is given by
F = rw dDmelt L f ; (2)
where rw = 1 kg m 3 is the density of liquid water. Hourly snow melt is calculated as the
difference between the potential and the actual snow water equivalent at the end of each hour,
dDmelt = Dpot Dact. The potential snow depth at the end of each hour is obtained by adding
the total hourly solid precipitation (snow
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf
caldera
covered by 150- to 250-m-thick ice (Figure
1). Its highest peak, Grímsfjall, on the southern
caldera rim, reaches an elevation of 1722 m.
Volcanic eruptions there, numbering several
per century, are phreatomagmatic because
of the ice cover, and they usually persist for
days to weeks. Geothermal activity continu-
ously melts the overlying ice, and meltwater
accumulates in a subglacial
/media/jar/myndsafn/2005EO260001.pdf
by the various models. In the large figure, months from Jan-
uary (1) to December (12) are depicted. On the right-top corner there is an enlarged illustration for
November-February, i.e., the months with the weakest incident radiation. Unit: MJ m−2 month−1.
analysis would corrupt the results severely. Therefore, the present analysis will be based
on 18 models, with the CSIRO model excluded.
Evaluation
/media/ces/CES_D2.4_solar_CMIP3.pdf