weather stations and manual observations
Ingibjörg Jóhannesdóttir51
1,0
2019-003
Hekla volcano monitoring project. Report to ICAO
Sara Barsotti, Michelle M. Parks, Melissa A. Pfeffer, Matthew J. Roberts, Benedikt G. Ófeigsson, Gunnar B. Guðmundsson, Kristín Jónsdóttir, Kristín S. Vogfjörð, Ingvar Kristinsson, Bergur H. Bergsson, Ragnar H. Þrastarson57
4,9
/about-imo/publications/2019/
compared with current
thinning regime, increased thinning thresholds
enhanced carbon stocks in Finland under current and
changing climate. This also enhanced timber
production during 2040-2069 (2nd period) and energy
wood production at final felling during 2040-2069
and 2070-2099 (3rd period).
Results
Contact info
The ecosystem model - Sima (Kellomäki et al., 1992a,
b; Kolström, 1998) was used
/media/ces/CES_BioFuels_Flyer_new.pdf
the winter, but weakens
and spreads northeast during the summer. The highest wintertime precipitation occurs southwest
10
Figure 3. Seasonal mean fields in winter ((a) and (c)) and summer ((b) and (d)). (a) and
(b): daily precipitation (coloured contours), 500 hPa geopotential height in metres (red
contour lines), and 250 hPa geopotential height (white contour lines). (c) and (d): sea
surface temperature
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
a debris cone in the run-out zone. The
source of the material is either within in the channel or in the talus slope above the channel.
Most of the landslides that occur in Strandartindur are debris flows of this type.
B Debris slides that are not confined to gullies and occur near a concave break of slope. The
main type of material is debris mixed with fine-grained material. Most of the landslides
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
support
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socia
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Farmers
,loca
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aut
horities
,
association
s
NO
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D
Cognitiv
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mappin
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HE
T
GM
B
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P
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T
Simulation
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o
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is
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io
n
su
pp
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Com
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unication
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Improv
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socia
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HE
/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
in the
21st Century
Evaporation change per Degree T change in the
21st Century
Runoff change per Degree T change in the 21st
Century
2) Downscaling
a) Statistical
b) Dynamical
Climate
Scenarios
Global climate
simulations, next
~100 yrs
Downscaling
Delta
Precip,
Temp
Hydrologic
Model (VIC)
Natural
Streamflow
Water
Management
Model
DamReleases,
Regulated
Streamflow
Performance
Measures
Reliability
/media/ces/Lettenmaier_Dennis_CES_2010pdf.pdf
size.
References
1. Meehl, G.A., C. Covey, T. Delworth, M. Latif, B. McAvaney, J.F.B. Mitchell, R.J. Stouffer and
K.E. Taylor, 2007: The WCRP CMIP3 Multimodel Dataset: A New Era in Climate Change Research, BAMS,
88, 1383-1394, DOI: 10.1175/BAMS-88-9-1383.
2. Naki �enovi � N., J. Alcamo, G. Davis, B. de Vries, J Fenhann, S. Gaffin, K. Gregory,
A.Grübler, T.Y. Jung, T. Kram, E.L. La Rovere
/media/ces/CES_D2.4_VMGO.pdf
Processes in South-West Iceland
Kristín S. Vogfjörd, Einar Kjartansson, Ragnar Slunga, Páll Halldórsson, Sigurlaug Hjaltadóttir, Gunnar B. Gudmundsson o.fl.
83 pp
3,2 Mb
2010-005
Surface Air Temperature and Precipitation Trends for Iceland in the 21st Century
Nikolai Nawri & Halldór Björnsson
42 pp
2,9 Mb
2010-003
Use of relatively located microearthquakes to map fault patterns
/about-imo/publications/2010/