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
average temperature change, the upper ranges of sea
level rise for SRES scenarios shown in Table 3.1 would increase by
0.1 to 0.2m.13 {WGI 10.6, SPM}
Table 3.1. Projected global average surface warming and sea level rise at the end of the 21st century. {WGI 10.5, 10.6, Table 10.7, Table SPM.3}
Temperature change Sea level rise
(°C at 2090-2099 relative to 1980-1999) a, d (m at 2090-2099 relative
/media/loftslag/IPPC-2007-ar4_syr.pdf
-scale Category
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Casualties and Timing
Casualties and Time of Day
150
200
250
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Fatalities
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50
100
Overnight Morning Early Afternoon Late Afternoon Late Evening
I
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Nocturnal Tornadoes
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8
9
10
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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
a procedure proposed by Peschke (1987). The
Richards-approach was used for modelling vertical water fluxes in the unsaturated zone, coupled
dynamically with a 2-D groundwater flow model for base flow generation. The hydraulic prop-
erties of the soil are parameterised according to Van Genuchten (1976). A module solving the
heat flux balance in the soil is available but had not yet been tested at the time
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf
Woodward,
A.-S. Mériaux, F. S. Tweed & M. Lim ().
The role of multiple glacier outburst floods in
proglacial landscape evolution: The Ey-
jaallajökull eruption, Iceland. Geology (),
–; doi: ./G..
Esther Hlíðar Jensen, Jón Kr. Helgason, Sigur-
jón Einarsson, Guðrún Sverrisdóttir, Ármann
Höskuldsson & Björn Oddsson (). Lahar,
floods and debris flows
/media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.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