water infra-
structure projects begun now are large
enough to push hydroclimate beyond the
range of historical behaviors (19). Some
regions have little infrastructure to buffer the
impacts of change.
Stationarity cannot be revived. Even with
aggressive mitigation, continued warming is
very likely, given the residence time of
atmospheric CO2 and the thermal inertia of
the Earth system (4, 20/media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf
The
American Political Science Review 97:233-243.
Jessop, B. 2005. The political economy of scale and
European governance. Tijdschrift voor Economische
en Sociale Geografie 96:225-230.
Katz, D., and I. Fischhendler. 2011. Spatial and
temporal dynamics of linkage strategies in Arab-
Israeli water negotiations. Political Geography 30
(1):13-24. doi:10.1016/j.polgeo.2010.12.002.
Kok, K., R. Biggs, and M
/media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf
Based on a report by
Verta et al. (2007)
92.
5
93.
0
93.
5
94.
0
94.
5
95.
0
M A MJ F J J A S O N D
Mean 19702000
Min and max 1970–2000,
natural rating curve
Target water level zone 1
Target water level zone 2
Q=+20%
Q=+10%
Q= 0%
Q=15%
Q=30%
92.90 m snow target 1
92.70 m snow target 2
Water level (m
)
Month
the regulation limits Lake Syväri has target water level zones, which are not legally
/media/ces/Water_resources_man_Veijalainen_etal.pdf
development:
Experiences from the SCENES project
Kasper Kok a,, Mathijs van Vliet a, Ilona Bärlund c, Anna Dubel b, Jan Sendzimir b
a Wageningen University, P.O. Box 47, 6700 AA Wageningen, Netherlands
b International Institute for Applied Systems Analysis, Schlossplaz 1, A-2361 Laxenburg, Austria
c Helmholtz Centre for Environmental Research (UFZ), Brückstrasse 3a, 39114 Magdeburg, Germany
a r t i c
/media/loftslag/Kok_et_al._TFSC_published_2011.pdf
by officers on site.
The restricted area extends 20 m outside the edges of the new lava field, to the edge of Dyngjujökull glacier on the south side, the river Jökulsá á Fjöllum to the east and to the westernmost branches of Jökulsá á Fjöllum in the west. Enlarge.
12 March 2015 - from the Scientific Advisory Board
Notes from the Meeting of the Scientific Advisory Board 10 March (pdf 0.3 Mb) are now
/earthquakes-and-volcanism/articles/nr/3122
by officers on site.
The restricted area extends 20 m outside the edges of the new lava field, to the edge of Dyngjujökull glacier on the south side, the river Jökulsá á Fjöllum to the east and to the westernmost branches of Jökulsá á Fjöllum in the west. Enlarge.
12 March 2015 - from the Scientific Advisory Board
Notes from the Meeting of the Scientific Advisory Board 10 March (pdf 0.3 Mb) are now
/earthquakes-and-volcanism/articles/nr/3122/