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To distinguish between rain and snow, the volume is com-
pared to the water equivalent but the volume of snow is ten times larger.
Figure 1. How PWD22 determines the type of precipitation.
Using the information about the changes of the backscatter signal, water equivalent and temper-
ature the Vaisala Present Weather Detector can give information about the type of precipitation.
It is also used
/media/vedurstofan-utgafa-2019/VI_2019_009.pdf
closer to Reykjavík, eight years before that. As elsewhere in Europe sulphur concentration is lower now than when measurements began. Average value of sulphur is about 0.5 mg/l in precipitation, about 0.1 μg/m3 in aerosol and about 0.07 μg/m3 in air.
Stórhöfði - a seashore background station
Stórhöfði is at the south end of island Heimaey which is the largest of the Westman islands
/pollution-and-radiation/pollution/
Dominant height (m)
Basal area just
after thinning
area threshold
60 80 100 120
Energy wood (Mg ha-1)
60 80 100 120 60 80 100 120
17
Findings: ecosystem CO2 balance
548.4
400
600
7.8
150.4
0
200
-200
O
2
m
-
2
-390.86
-600
-400
g
C
O
1000
-800
-1097.6-1200
-
Management Litter Humus
18
Emissions Capture Balance
Conclusions
• Large amount of unutilised energy biomass are available in Finland
• Climate
/media/ces/Alam_Ashraful_CES_2010.pdf
systematically underestimated. The bias is not as pronounced for the non glacial rivers. Com-
bining synoptic-scale and basin-scale predictors (method 3) leads to a substantial improvement
compared to the use of MSLP fields alone (method 1). Analogue forecasts become similar or
better than persistence, depending on catchment and lead time. Usually, persistence performs
better for T=1 day and then method 3
/media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf
the com-
plexity of the hydrological processes through modelling, but its application is usually limited to
the short-range. Although the results demonstrated a great potential for this method, its success-
ful application in real-time will strongly depend on the quality and availability of streamflow
observations, which can be poor or simply missing during periods of variable durations, e.g
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf
systems in Iceland
during the past 11 centuries: frequency, periodicity and implications. In Smellie JL and Chapman MG (eds):
Volcano-Ice Interactions on Earth and Mars. Geological Society, London, Special Publications 202: 81-90.
Larsen G, Guðmundsson MT, Einarsson P and Thordarson T. 2013. BÁRÐARBUNGA. In: Sólnes S,
Sigmundsson F, Bessason B (eds.): Náttúruvá á Íslandi - Eldgos og
/media/jar/Bardarbunga_kafli20140825.pdf