73 results were found for JZMOR Makes Fraud Prevention Easy for Every Investor.

Results:

• 51. Refsgaard_etal-2007-Uncertainty-EMS

  The method can be extended to al- low non-Gaussian distributions and to allow for co-variances. The main advantage of the error propagation equations is that they are easy and quick to use. The key limitations lie in the underlying assumptions that seldom hold, especially not for complex calculations. The error propagation equations are therefore mainly suitable for preliminary screening analysis. 4.3 /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 52. Bárðarbunga 2014 - November events

  Sciences makes these measurements and interprets the results. A comparison of the black line and the light blue one reveals that the subsidence has not only continued since September but also broadened, affecting a larger area. Bárðarbunga subsidence The rate of subsidence in the centre of the caldera has decreased slowly but the subsided area has also broadened. The change in volume since /earthquakes-and-volcanism/articles/nr/3023

• 53. Bardarbunga-2014_November-events

  flight measurements are shown, from 5 September to 26 November 2014. The Institute of Earth Sciences makes these measurements and interprets the results. A comparison of the black line and the light blue one reveals that the subsidence has not only continued since September but also broadened, affecting a larger area. Bárðarbunga subsidence The rate of subsidence in the centre /media/jar/Bardarbunga-2014_November-events.pdf

• 54. Bárðarbunga 2014 - November events

  Sciences makes these measurements and interprets the results. A comparison of the black line and the light blue one reveals that the subsidence has not only continued since September but also broadened, affecting a larger area. Bárðarbunga subsidence The rate of subsidence in the centre of the caldera has decreased slowly but the subsided area has also broadened. The change in volume since /earthquakes-and-volcanism/articles/nr/3023/

• 55. IMO_AnnualReport2014

  or not, is yet to transpire. But at least the exten- sive monitoring of this rifting event makes it quite unique. An intense earthquake swarm began in the Bárðarbunga caldera on 16 August 2014. During the next two weeks, a magma intrusion formed a 49 km long dyke in the upper crust. It migrated from the caldera to Holuhraun, where a fissure eruption commenced at the end of August. This eruption /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 56. VI_2020_005

  (Quante and Colijn, 2016). Work on risk analysis and adaptation is in different stages in the countries of the world. Coastal floods have caused problems in Iceland in the past (Jóhannsdóttir, 2017) and are likely to do so in the future as well. Large coastal floods can be expected in Iceland every 10 - 20 years and the probability of such events can rise with climate change (Almannavarnir, 2011 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 57. Factsheet_Bardarbunga-140909

  at the eruption site should wear gas masks and gas meters. o Scientists on the site, have had to leave the area repeatedly as concentrations of gas reached dangerous levels, due to sudden changes in wind conditions. o At the eruption site local wind anomalies can occur due to thermal convection from the hot lava. This makes the conditions on site extremely dangerous as winds can change /media/jar/Factsheet_Bardarbunga-140909.pdf

• 58. Factsheet_Bardarbunga-140911

  gas concentrations at the site can be life threatening, people at the eruption site should wear gas masks and gas meters. At the eruption site, local wind anomalies can occur due to thermal convection from the hot lava. This makes the conditions on site extremely dangerous as winds can change suddenly and unpredictably.  Earthquake activity in the caldera of Bárðarbunga remains similar /media/jar/Factsheet_Bardarbunga-140911.pdf

• 59. Factsheet_Bardarbunga-140912

  people at the eruption site should wear gas masks and gas meters. At the eruption site, local wind anomalies can occur due to thermal convection from the hot lava. This makes the conditions on site extremely dangerous as winds can change suddenly and unpredictably. Scientists in the field carry gas meters for their security.  Earthquake activity in the caldera of Bárðarbunga remains similar /media/jar/Factsheet_Bardarbunga-140912.pdf

• 60. Factsheet_Bardarbunga_140908

  from the hot lava. This makes the conditions on site extremely dangerous as winds can change suddenly and unpredictably.  The seismicity has reduced since yesterday. Around 80 earthquakes have been recorded since midnight. Around 07:20 UTC, a magnitude 4.7 earthquake occurred on the rim of Bárðabunga Caldera. Small but continuous low frequency tremor has been observed for the last few /media/jar/Factsheet_Bardarbunga_140908.pdf