station Region type Catchment area,
Q station (km2)
Lake percentage
(%)
Settlement for
inundation analysis
Boundary conditions
of the 2D model
a Köngäs Ounasjoki Small/medium,
northern river
4488 4.2 Kittilä Upstream : Q; Downstream : river WSE
b Sonkajärvi Small, lake 946 4.4 – –
c Keppo Lapuanjoki Small/medium,
coastal river
3949 3.0 Lapua Upstream : Q; Downstream river WSE
d Harjavalta
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
Steinunn S. Jakobsdóttir & others - Opening address
08:55 Ragnar Stefánsson - From earthquake prediction research to useful warnings ahead of earthquakes
09:20 Ragnar Slunga - Microearthquakes, stresses, crustal stability, and earthquake warnings
09:45 Reynir Bödvarsson - Development history and future potential of the SIL system
10:10 Coffee and posters
10:50 Halldór Geirsson & others
/earthquakes-and-volcanism/conferences/jsr-2009/schedule/
acceptance, we
request a copy of the final manuscript, and as
many figures as possible, on a computer
diskette. It is essential that the name and
version of the word processing program and
computer type, is included on the diskette.
Preferred software formats are LaTex or MS
Word. The editors also welcome an ascii-text
version of the final manuscript in electronic
mail. Short to moderate
/media/jar/Jokull-guidlines.pdf
behavior towards
a public good based on individual preferences, and provides insights into the type of indi-
viduals who best serve the social interest and those to avoid in institutional settings. This
distinction helps us to understand why, with the same incentives, the provision of public
goods works better in some populations than in others. In addition, our use of a sequential
public good
/media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf
in Iceland: Climate projections and historical changes in precipitation type Andréa-Giorgio R. Massad, Guðrún Nína Petersen, Halldór Björnsson, Matthew J. Roberts & Tinna Þórarinsdóttir99
20,6
/about-imo/publications/2022/
Amplitude Measurement (RSAM) data are one of the most
important tools utilized in volcano observatories worldwide. The IMO’s monitoring office is
no exception, as this type of real-time data shows mid- to long-term trends, which is especially
important for monitoring active volcanic systems. The RSAM methodology was developed by
the USGS in 1989 (Murray & Endo, 1989) to plot averaged amplitude
/media/vedurstofan-utgafa-2021/VI_2021_008.pdf
For the classification of wind
conditions, wind direction over the lake is rounded to the nearest 45 degrees.
area covered in the model with sparse tundra (41.3% of the model land area) is in fact bare
rock or sand plains. The model description of surface type is therefore not a likely cause for the
strong wintertime cooling, since replacing at least sparsely vegetated areas in the interior of the
island
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
such as
irrigation, CO2 effects on transpiration, and land use changes affect the water balance to a
lesser extent.
Citation: van Roosmalen, L., T. O. Sonnenborg, and K. H. Jensen (2009), Impact of climate and land use change on the hydrology of
a large-scale agricultural catchment, Water Resour. Res., 45, W00A15, doi:10.1029/2007WR006760.
1. Introduction
[2] The most recent Intergovernmental Panel
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf