81 results were found for Protezione avanzata JZMOR per prevenire ogni tipo di truffa.

Results:

• 71. Mapping water resources in the Nordic region under changing climate

  number of days per year with snow covered ground, and annual maximum soil moisture deficit. Partners CICERO, Center for Klimaforskning, Norway Denmark Meteorological Institute Ea Energianalyse A/S, Danmark /ces/research/mapping/

• 72. Articles

  release per week and the right panel the weekly number of events of magnitudes M1-2 (blue), M2-3 (green) and M>3 (red). Both lower panels show the activity on the caldera rim, moment on the left and event numbers on the right, here the colours for the event numbers are here M3-4 (blue), M4-5 (green) and M>5 (red). Please notice that the last data point in all plots represents the ongoing week /earthquakes-and-volcanism/articles/bigimg/3039

• 73. Bardarbunga_daily_status_report_31082014

  extruded. At 07 AM the lava flow was around 1 km wide and 3 km long towards northeast. The thickness was estimated a few meters, the flow rate about 1000 m3 per second. There has been poor visibility until 11:30 UTC, then it has been moderate. The eruptive fissure is visible since then and magma extrusion is still ongoing. White steam rising from the eruption is also visible. Seismic tremor /media/jar/Bardarbunga_daily_status_report_31082014.pdf

• 74. Eyjafjallajokull_status_2010-05-18_IES_IMO

  Lightning: More than 70 lightning strikes from midnight to midday (up to 10 flashes per hour until noon but has deacresed in the afternoon) have been detected. Noises: No reports. Meltwater: Low water discharge at Gígjökull. Conditions at eruption site: No direct observations of the eruption site today. The plume has been mostly steady at 7 km height. The size, height and colour of the plume /media/jar/Eyjafjallajokull_status_2010-05-18_IES_IMO.pdf

• 75. norsem_martin

  for the time period 2001–2009, obtained from the permanent SIL network, were analysed to study stress changes associated with the main shocks. Results reveal a coseismic counter-clockwise rotation of the maximum horizontal stress of 11 ± 10° (95 per cent confidence level) in the main rupture region. From previous fault models obtained by inversion of geodetic data, we estimate a stress drop /media/norsem/norsem_martin.pdf

• 76. CES_D2_2_poster_3x3

  in 1971-2000. Best estimates of precipitation change. Top: precipitation changes for the decade 2011-2020 in four three-month seasons. Bottom: annual mean precipitation change as a function of time, from 2011-2020 to 2041-2050. All changes are expressed in per cent of the mean precipitation in 1971-2000. HOW CERTAINLY WILL TEMPERATURE AND PRECIPITATION INCREASE? Probability of warming is very /media/ces/CES_D2_2_poster_3x3.pdf

• 77. VED_AnnualReport-2013_screen

  ; from which extensive data streams enter IMO and are utilized for forecasts and research purposes. Dissemination The main dissemination of IMO is in the form of forecasts and warnings; through radio, T V, direct di- alog with stakeholders and through IMO‘s web-site (vedur.is). Additionally, the web provides compre- hensive real-time data on the weather, earthquakes and deformation, as well /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

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

  to 1.3 cm over one year. In the spring of 2018, a new fracture running down the western slope of Svínafellsheiði was discovered. Recent analysis of remote sensing data shows that the area between the fractures and the glacier margin has moved at a rate of 2 to 4 cm per year in the period from late August 2016 to late August 2017. The area in motion is about 0.5–1 km2 in size. A rough estimate /about-imo/news/fractures-in-svinafellsheidi-and-a-potential-rockslide-on-svinafellsjokull

• 79. More

  earthquake activity north of GrindavíkRecent data show that uplift has started again, with the center just west of Mt. Thorbjorn. Uplift was measured from 22. January 2020 until beginning of February and has started up again during the first half of March. During the first sequence in January-February, the deformation rate was about 3-4 mm per day with a total of a 6 cm uplift during the whole /about-imo/news/more-research-is-needed-to-decipher-the-on-going-activity-at-the-reykjanes-peninsula-as-a-whole

• 80. Ice surface lowering - striking graph

  For latest information, see Remarks of a specialist (in red) on the Hydrology front page. Background Jökulhlaups in Skaftá are sourced from two ice cauldrons, formed due to persistent geothermal activity beneath Vatnajökull. On average, the cauldrons drain every two years, producing floods of up to 1,500 cubic metres per second. When the interval between floods is short the flood tends /about-imo/news/nr/3203