The recent Bothnian Bay M4.1 earthquake: where, how and why?
B. Lund1, M. Uski2, H. Shomali1, D. Buhcheva1, S. Amini1, J. Kortström2
1Dep. of Earth Sciences, Uppsala University, Sweden
2Institute of Seismology, Dep. of Geosciences and Geography, University of Helsinki, Finland
On 19 March 2016 a magnitude 4.1 earthquake occurred in the Bothnian Bay, between northern
Sweden
/media/norsem/norsem_lund.pdf
example
can be given by the low cost still flood risk adaptation by implementing early warning system. But
there is one more suggestion dfor stakeholders to restrict infrastructure in the cities of Horsens.
Fiva PhD Courses : Adaptive management in relation to climate change (august 22 2011 - august 26 2011)
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/media/loftslag/Group-1_Scenarios-for-AWM.pdf
Tengö, D. Timmer,
and M. Zurek. 2007. Linking futures across scales:
a dialog on multiscale scenarios. Ecology and
Society 12(1): 17. [online] URL: http://www.ecolog
yandsociety.org/vol12/iss1/art17/.
Borgatti, S. P., and P. C. Foster. 2003. The network
paradigm in organizational research: a review and
typology. Journal of Management 29(6):991-1013.
Brenner, N. 2001. The limits to scale
/media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf
(a) annual maximum temperature (b)
and annual minimum temperature (c) as simulated by the ensemble of 9 CMIP3 AOGCMs for
2046-2065 relative to 1980-1999. Units are K. Dots denote grid boxes for which signal-to-noise
ratio is greater than 1.
a)
b)
c)
d)
Fig.2 Same as in Fig.1 but for changes in heat (a) and cold (c) wave
/media/ces/CES_D2.4_VMGO.pdf
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/media/loftslag/Tornado_Impacts_-_FMI_Presentation.pdf
of stationarity was
Climate change undermines a basic assumption
that historically has facilitated management of
water supplies, demands, and risks.
Stationarity Is Dead:
Whither Water Management?
P. C. D. Milly,1* Julio Betancourt,2 Malin Falkenmark,3 Robert M. Hirsch,4 Zbigniew W.
Kundzewicz,5 Dennis P. Lettenmaier,6 Ronald J. Stouffer7
CLIMATE CHANGE
1U.S. Geological Survey (USGS), c/o National Oceanic
/media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf
to theoretical framework. I do also want to thank him for an
enjoyable time during this work, both in the office and in the field.
This work was carried out as a part of the Skaftá cauldrons research project which
was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja-
sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com-
pany), the National Energy
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
in the volcanic cloud. The more abundant gases present are
SO2, CO2, HCl, HF, H2O.
In the first month and half we had an averaged flux equals to 400 kg/s (~35 kT/d) with peaks up to 1300
kg/s (~112 kT/d). Assuming a constant release of gas until today, the eruption has injected into the
atmosphere an amount of SO2 in the range 3.5 Mt (considering the average flux) – 11.2 Mt (considering
the peak
/media/jar/bb100days_ens.pdf
)
Best case (1.5 C increase; 2%
increase in prec)
BAU A B
Change +30 % C D
Scenario
combination
Impact
Adaptation measures
North South North South
A *
CC: Possible increase in the
amount of snow more
snow clearing increase in
operational costs
S-E: increase in traffic
volume increased wear of
roads increase in
maintenance cost.
**
CC: Possibly less snow,
more rain
/media/loftslag/Group3-The-future-of-the-Finnish-national-road-network.pdf