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
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
in Finland
Noora Veijalainen a,*, Eliisa Lotsari b, Petteri Alho b, Bertel Vehviläinen a, Jukka Käyhkö b
a Freshwater Centre, Finnish Environment Institute, Mechelininkatu 34a, P.O. Box 140, FI-00251, Helsinki, Finland
b Department of Geography, FI-20014 University of Turku, Turku, Finland
a r t i c l e i n f o
Article history:
Received 7 January 2010
Received in revised form 13 June 2010
Accepted
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
was funded mainly by the National Avalanche and Landslide Fund, with additional financial contributions from the Icelandic Road and Coastal Administration and the National Power Company.
Published material
Under the link below, each of the chapters can be downloaded or short summaries read.
Pagneux, E., Gudmundsson, M. T., Karlsdóttir, S., & Roberts, M. J. (Eds.) (2015). Volcanogenic floods
/hydrology/hazard-risk-assessments/glacial-outburst-floods/markarfljotsaurar-oraefajokull/
values
t
mean temperature
tx
average daily maximum temperature
txx
highest maximum temperature month/year
txx_dag1
date of highest maximum temperature
tn
average daily minimum temperature
tnn
lowest minimum temperature month/year
tnn_dag1
date of lowest minimum temperature
rh
mean relative humidity
r
preciptiation total
rx
maximum 24-hour precipiation
/climatology/data/
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/
model errors discussed in the previous section, a model time-series
of 2-m temperature or 10-m wind speed, Mi(t), interpolated to the i-th station location, can be
linearly transformed such that the mean square error compared with the local station time-series
is minimised. Generally, the corrected time-series is then given by
M˜i(t) = ai Mi(t)+bi ; (2)
where at each station location, the correction
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
Agenda
*All presentations will be in the Forgardur (forecourt) underground basement room of the IMO
building at Bustadavegur 7, unless otherwise noted.
Wednesday, 13 November
Time Agenda Item
09:00 – 09:15 Welcome and Introductions
- T Jónsson and E Hanna
09:15 – 09:30 Meeting Structure and Overview
- J Overland and E Hanna
09:30 – 10:40
09:30 – 09:45
09:45 – 10:05
10:05 – 10:25
/media/loftslag/Mid-Latitudes-Agenda1_nov2013EH.pdf