versa
• Very large range within the simulations
• Larger number of observation stations in the study area leads to
• better compatibility between different observational data sets
• smaller bias in the model simulations
CES Conference, Oslo 31.5.-2.6.2010
References
• Haylock, M. R., Hofstra, N., Klein Tank, A. M. G., Klok, E. J., Jones, P.
D. and New, M. 2008. A European daily high-resolution
/media/ces/TietavainenHanna_CES_2010.pdf
on the
Shifts of climatic
zones from
cooler or wetter
to warmer or
drier
(a) 1971-2000 (b) 2010-39 A1B
observational data set
(0.25º grid) from Haylock
et al. (2008)
(b-d) Based on CMIP3
GCM runs for A1B
& the delta-change
method
(c) 2040-69 A1B (d) 2070-99 A1B
Jylhä et al. (2010)
Uncertainties in climate change schematically
Observed
climate
Future
climate Natural
/media/loftslag/Case_B___Road_transport_operation_and_infrastructure_planning.pdf
We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below:
A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö
A
A: Icelandic abbreviation of East (compass direction, easterly, eastern).
ANA: Icelandic abbreviation of Eastnorthesast (compass direction).
ASA: Icelandic
/weather/articles/nr/1208
We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below:
A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö
A
A: Icelandic abbreviation of East (compass direction, easterly, eastern).
ANA: Icelandic abbreviation of Eastnorthesast (compass direction).
ASA: Icelandic
/weather/articles/nr/1208/
the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits
were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes
evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob-
servations
/media/ces/GA_2009_91A_4_Andreassen.pdf
to use the available new estimates
Mw(v) to build a PGA relationship that would give very similar results as model A. Due to the
more complicated relationship between Ci and Mw(v) in the acceleration case, a second order
polynomial was chosen as the functional form of h and thus through the least-squares method
we estimated the parameters b, c and d according to:
Ci = d·Mw2(v) + b·Mw(v) + c
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf
level, surveys commissioned by the European Com-
munity/the European Union provide an indication of trends in concern about cli-
mate change. Since 1992, such surveys have been undertaken among representative
samples of citizens in its Member States, and specifically on topics related to the
environment (Special Eurobarometers (EB) in 1992, 1995, 2002; and a Flash EB
in 2002). These have included
/media/loftslag/Lorenzoni_Pidgeon_2006.pdf
the volcanic
plume due to their size and weight fall close to the volcano and constitute the
proximal deposit. Smaller particles can reach higher altitudes and persist in the
atmosphere for days and weeks and be advected far away by the wind. This
fraction of the pyroclastic material can possibly generate a distal deposit
very thin and covering wide areas.Term Size Ballistic d > 64 mm Lapilli 2 mm < d/volcanoes/volcanic-hazards/volcanic-emissions/