68 results were found for JZMOR: Your Shield Against Online Scam and Fraud Risks.

Results:

• 61. Risk Assessment and Stakeholder Involvement

  presentations both on theory & methods and on case studies will be given. Background Climate change will cause major effects for many sectors. Adaptation to future changed climate poses large and complex challenges as well as opportunities for societies, whereas solutions may often entail trade-offs between sectors, areas, social groups, and various risks. For these reasons decision making /nonam/workshop/

• 62. Abstract_Impacts_of_Climate_Change_on_Stormwater_Systems_in_Reykjavik

  the method with new data (1985-2008), 10 minutes design intensity increased by 16%. An increase in short term extreme precipitation may increase the risks of flooding in stormwater systems. The inconveniences are expected to be greatest in the older parts of towns with combined sewer and rainwater collections systems. These increased risks will be investigated in downtown Reykjavík. Modeling /media/loftslag/Abstract_Impacts_of_Climate_Change_on_Stormwater_Systems_in_Reykjavik.pdf

• 63. Kok_et_al._TFSC_published_2011

  l e i n f o a b s t r a c t Article history: Received 30 November 2009 Received in revised form 11 January 2011 Accepted 14 January 2011 Available online 17 February 2011 Social, natural and cultural systems are changing rapidly, influencing the future of Europe's fresh waters. One of the drivers shaping this future is the implementation of the Water Framework Directive. Participatory scenario /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 64. FAQ

  can the eruption be expected to last? A direct connection has now been established from the mantle to the surface in Geldingadalir. Primarily, it is the amount of available magma at the boundary of the crust and mantle that determines how much material eventually reaches the surface. There are examples of shield volcanic eruptions on the Reykjanes Peninsula that lasted for many years /volcanoes/fagradalsfjall-eruption/faq/

• 65. Ved-eng-2006

  An extensive grass fire was raging for a few days in the west, starting on 30 March. This grass fire is the largest known in Iceland, about 67 sq kilometers (6700 hectares) were burned. The squads fighting the fire managed to shield all farmhouses in the very sparsely populated area. The area will presumably recover in a few years as there is no forest there. Reykjavík /media/vedurstofan/utgafa/skylduskil/Ved-eng-2006.pdf

• 66. Fractures in Svínafellsheiði and a potential rockslide on Svínafellsjökull

  ). Fractures in Svínafellsheiði and a potential rockslide on Svínafellsjökull Civil Protection advises against travel on Svínafellsjökull 22.6.2018 In the autumn of 2014, a surface fracture was discovered /about-imo/news/fractures-in-svinafellsheidi-and-a-potential-rockslide-on-svinafellsjokull

• 67. Supporting structures stopped most of an avalanche

  the mountainside (see fig. 1). An avalanche slab was released inbetween the rows of supporting structures. The snow was mostly stopped by the structures and piled up against them (see fig. 2) but part of the snow jumped over the rows. A slab was also released below the lowermost row. The avalanche stopped near the foot of the slope to the west of the structures but before it reached the bottom of the slope /about-imo/news/nr/2476

• 68. Supporting structures stopped most of an avalanche

  near the mountainside (see fig. 1). An avalanche slab was released inbetween the rows of supporting structures. The snow was mostly stopped by the structures and piled up against them (see fig. 2) but part of the snow jumped over the rows. A slab was also released below the lowermost row. The avalanche stopped near the foot of the slope to the west of the structures but before it reached the bottom /avalanches/articles/nr/2475