). This can be helpful with respect to
finding a common structure in presenting as well in session reporting (for which angles
mentioned in the opening session statements of the Workshop participants can provide
checkpoints).”
Session rapporteur allocation
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/media/loftslag/Guidelines2-for-rapporteurs.pdf
publ.25/2008,
pp.75-126.
Venäläinen, A. and Kangas, M. (2003), Estimation of winter road maintenance costs using climate data,
Meteorological Applications, Vol. 10, pp.69–73
NONAM PhD course – Adaptive management in relation to climate change – Copenhagen 21-26/8/2011
……………………………………………………………………………………………………………………………………………………………………
9
Transport case – questions and tasks
The case
/media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf
in estimating the height of the plume. At this time, the plume reached heights of 8 - 12 km.
During the 2010 Eyjafjallajökull eruption, the weather radar proved to be a very useful tool, but the great distance to the eruption site (160 km) reduced the quality of the data. Therefore, a mobile X-band weather radar was purchased, but while this custom made radar was being assembled and tested, another
/about-imo/news/nr/2183
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7 78 Anja Wejs Denmark
Environmental
management
8 93 Tommy Chan Finland Forest sciences
9 140 Karoliina Pilli-Sihvola Finland
E viro me tal
economics
10 147 Jussi Ylhäisi Finland Meteorology
11 (new) Karen Lundgren Sweden
Engineering &
Design
12 (new) Väinö Nurmi Finland Economics
13
/media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
; in particular Chapter 4).
7 Seppo Saarelainen & Lasse Makkonen: Adaptation to climate change in the road management – Pre-study.
Helsinki 2007.
8 The Finnish Road Administration (Finnra) (2009), The effect of climate change on the routine and periodic
maintenance of roads, Finnra report 8/2009, (in Finnish, abstract in English).
9 Salanne, i., Byring, B., Valli, R., Tikkanen, R., Peltonen, P
/media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf
the radar backscatter signal recorded at 14:20 hrs on 23 May 2011. Also, the maximum backscatter in the vertical plane is shown, which can be used in estimating the height of the plume. At this time, the plume reached heights of 8 - 12 km.
During the 2010 Eyjafjallajökull eruption, the weather radar proved to be a very useful tool, but the great distance to the eruption site (160 km) reduced
/about-imo/news/nr/2183/
-scale Category
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Casualties and Timing
Casualties and Time of Day
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Nocturnal Tornadoes
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/media/loftslag/Tornado_Impacts_-_FMI_Presentation.pdf