and
calculated travel time differences for pairs of closely spaced earthquakes observed at a series of
recording stations. Each earthquake is paired with several other earthquakes and the best fitting
distances between them as a group are determined. Methods based on this kind of minimization are
called double-difference (DD) earthquake location algorithms
/media/norsem/norsem_begga.pdf
model. Our estimates are derived from a) three pairs of photographs from 1891 and
2011, b) geomorphological field evidence delineating the maximum glacier extent at the end
of the Little Ice Age, and c) the high-resolution digital elevation model from 2010–2011. The
historical photographs of Frederick W.W. Howell from 1891 were taken at the end of the
Little Ice Age in Iceland, thus providing
/media/vatnafar/joklar/Reykholt-abstracts.pdf
compiled by using i) aerial photographs taken between 1979 to 1984 by the
American Defense Map Agency (DMA) and the Icelandic Geodetic Survey, ii) airborne
EMISAR radar images obtained in 1998 by the Electromagnetic system (EMI) of the
Technical University of Denmark, and iii) two image pairs from the SPOT 5 high resolution
stereoscopic (HRS) instrument from 2004. The ice-free part of the EMISAR
/media/ces/glacier_mass_balance_poster.pdf
Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009
ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost
operating manage- ment develop- poned-, of land grants ons European tax over- level
costs ment ment comprehen- build- and com- Regional De- heads
1991- 1991- sive- and ings pensation
/media/loftslag/Traffc-maintenance_expenditures.pdf
of the SPOT5 stereo
image pairs at some sections in the accumulation area of
Hoffellsjökull, were filled by smoothly adjusting the LiDAR
Fig. 3. A topographic relief shading showing the August 2010 Li-
DAR DEM of the terminus and the lower part of Hoffellsjökull. The
LIA terminus moraines can be seen in front of the terminus as well
as the extensive break-up of the eastern branch of the terminus
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
/lexuriserv/lexuriserv.do?uri=com:2007:0002:FIN:EN:PDF, 13
April 2009.
[2] WTO, World Tourism Organization (2008): “Climate Change and Tourism -
Responding to Global Challenges”, UNWTO, 9 July 2008, Madrid, Spain.
Available at:
http://www.unwto.org/media/news/en/press_det.php?id=1411&idioma=E, 7
March 2010.
[3] Mooney, J.E. y Miller, M.L. (2009): “Climate change: Creating demand for
sustainable
/media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.pdf
and
watershed scale
Statistical downscaling
Dynamical downscaling
3) Hydrological and water resources
implications -- examples
4) Weak links and the path forward
1) Projected global and regional
runoff changes
Median runoff sensitivities per degree of global warming,
from 68 model pairs – 30-year model average runoff minus
1971-2000 model average (23 models, 3 global emissions
scenarios)
51
/media/ces/Lettenmaier_Dennis_CES_2010pdf.pdf
periods that share practically the same multi-model global mean temperature change as
simulated between 1961-1990 and 2021-2050 (1.35°C) can be taken as plausible realizations
of the climate change that could occur between 1961-1990 and 2021-2050. Sub-sampling the
latter 30-year period with 5-year interval, 12 such pairs of periods (from 1910-1939 / 2011-
2040 to 2021-2050 / 2066-2095
/media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf