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
that, the detrended timeseries would have had a net difference of
zero if the negative values had not been set back to zero. This shows that over the 39 years of
data, there was a slight precipitation increase for this grid-point. This trend has been removed,
resulting in a detrended, almost flat dataset.
29
Figure 14. Regression lines for hourly precipitation timeseries of grid-point [100, 100]
from
/media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf
grundvelli myndatöku með
flygildum og leysimælitæki (TLS) hefur verið notað við kortlagningu
flóðfara og við mat á útbreiðslu og umfangi hlaupa.
Þétt net jarðskjálftamæla, sem staðsettir eru á jökulskerjum eða
grafnir í jökul, hefur gefið góða raun við ákvörðun á dýpi jarðskjálfta
undir jöklum. Kvikuhreyfingar hafa þannig verið kortlagðar og
myndun gosrása staðfest af meiri nákvæmni en áður. Þó
/media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.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