73 results were found for ������pk10-���������������������360bet.net���������-������������1���������350-���������������������������������������-���������������������sogou7.com���������-������pk10-������pk10-������������������������������-���������������������bet91.net���������.
in the legend (left part of the map) and in the figure caption (the phrase below the map). The colour scale reports different values of likelihood (under 1% has no colour).
The maps have been made considering 10 years of meteorological data and computing the ground concentration each hour with the CALPUFF gas dispersion model. The results have been plotted considering the wind variability across
/pollution-and-radiation/volcanic-gas/hazard-zoning
and provide a narrative approach for tool enhancement.
r 2007 Elsevier Ltd. All rights reserved.
Keywords: Groundwater management; Bayesian belief networks; Qualitative interview; Adaptive management; IWRM; Tool enhancement; Participatory
integrated assessment; Social learning; Newater; Organizational complexity
1. Introduction and indexes are available e.g. poverty index, water stress
index etc
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
flooding, sea level, sea level rise, risk assessment, natural hazard
This work was carried out for the Icelandic Meteorological Office and is a part of Masters Thesis ISSN
1650-6553 No. 470, published by the Department of Earth Sciences at Uppsala University in 2019. The
Masters Thesis is available as a whole at www.diva-portal.org.
Copyright c Guðrún Elín Jóhannsdóttir
Contents
1 Introduction
/media/vedurstofan-utgafa-2020/VI_2020_005.pdf
changes in many natural
systems. Moreover, it also presents, in a greater or lesser extent, economical effects in
nearly every sector of activity. In this context, the tourism will be particularly affected
[1; 2]. There will be regional and seasonal shifts in global tourist flows, leaving some
countries more vulnerable to shifting climatic conditions [3]. European Mediterranean
countries
/media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.pdf
26.8.2011Adriaan Perrels/IL 6
Review of climate change effects in built-up areas (1)
Source:
IPCC 4AR_2
Source: IPCC 4AR_2
26.8.2011Adriaan Perrels/IL 7
Source: IPCC 4AR_2
Review of climate change effects in built-up areas (2)
26.8.2011Adriaan Perrels/IL 8
Cost-benefit analysis – the basics 1
• CBA:
• assess for the estimated lifetime of a project the annual expenditures
(investment funding cost
/media/loftslag/Perrels-CBA.pdf
are photographs, maps and graphs that show the main results of measurements
and analyses that are available, now two weeks after the event.
Width of fracture line: 800 m
Vertical drop: 350 m
Runout length beyond the lake shore: ~1000 m
Volume: ~30–50 million m³
Estimated duration of the slide: 20 seconds according to seismographs
Travel time of tsunami across the lake: 1–2 minutes
/media/ofanflod/myndasafn/frodleikur/askja_minnisblad_ens.pdf
Introduction
Electricity system model
Simulation results
Summary and concluding remarks
Energy systems
Quantitative analysis of the NordPool electricity system
Birger Mo, Ove Wolfgang, Joar Styve
Sintef Energy Research
02.06.2010
Sintef Energy Research Quantitative system analysis 1 of 21
Introduction
Electricity system model
Simulation results
Summary and concluding remarks
Outline
Methodology
1/media/ces/Mo_Birger_CES_2010.pdf
the discharge in Skaftá and the
temperature of the flood water close to the glacier margin were measured. The dis-
charge from the subglacial lake during the jökulhlaup was calculated using a hypso-
metric curve for the subglacial lake, estimated from the form of the surface cauldron
after jökulhlaups. The maximum outflow from the lake during the jökulhlaup is esti-
mated as 123 m3 s 1 while
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
plume rise up above Askja at 23:27. The steam plume was created when the slide exposed shallow geothermal areas in the release area. In addition, a dust cloud created by the rock slide may have contributed to the plume.
The release area of the rockslide is approximately 800 m wide and 350 m above the lake surface. It may have been a "rotational slide movement", which means that the failure surface
/avalanches/articles/nr/2929
....................................................................................................................................... 9
Ágrip ......................................................................................................................................... 11
1 General introduction ........................................................................................................... 13
1.1 Main aim of the project
/media/vedurstofan-utgafa-2020/VI_2020_004.pdf