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74 results were found for WA 0812 2782 5310 Order Meja Ukuran 1 Meter Jenawi Karanganyar.


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  • 31. Re-evaluation needed of the size of the hazard area

    at midnight on the 6th of April and is between the two existing fissures. Rescue teams from the Icelandic Association for Search and Rescue had detected subsidence in the area on the 6th of April about 420 meters northeast of the original eruption area in Geldingadalir, which was about 150m long and about 1 meter deep. In the photos that were taken during the reconnaissance flight on the 7th /about-imo/news/new-fissure-near-the-eruption-site-in-geldingadalir
  • 32. Group2-report

    1    Adaptive management to climate change in Horsens Fjord using scenario  development    Report by Maria, Azhar, Bjarke and Kerstin  Introduction  Horsens Fjord is an eutrophic estuary situated in east coast of Jutland, Denmark with approximately 46 km2  surface area. The Fjord is a part of bigger WFD catchments area with dominated agriculture area and small  forest, wetlands, lakes, and urban /media/loftslag/Group2-report.pdf
  • 33. Ash measurements

    1 2 Ash measurements 24.5.2011 Recently, the IMO obtained a LIDAR (Light Detection and Ranging) on loan from /about-imo/news/nr/2183
  • 34. Group4

    loop learning and innovation. The original remit was to analyze the projected climate change impacts on the projected needs for road maintenance on Finnish national road network while maintaining existing levels of service. However, in light of the need to radically reduce transport sector GHG emissions in order to keep average global warming under a 2 degree threshold (IPCC, 2007 /media/loftslag/Group4.pdf
  • 35. Supercomputer in Iceland

    Supercomputer in Iceland DMI - IMO partnership 21.5.2016 A new and highly effective supercomputer is up and running at Bústaðavegur 7 in Reykjavík. In order to fulfill environmental requirements, the Danish Meteorological Institute (DMI) approached the Icelandic /about-imo/news/nr/3309
  • 36. Öræfajökull – frequent questions & answers

    to melt. The pyroclastic flows and jökulhlaup caused by the 1362 eruption are thought to have resulted in the death of ~300 individuals. The magnitude of the 1362 jökulhlaup was of order 100,000 m3/s, whereas the 1727 flood was about half that size. In 1362 tephra fallout buried houses and villages with a deposit >40cm thick.The Öræfajökull eruption in 1362 has been one of the largest eruption /volcanoes/about-volcanoes/oraefajokull/q-a/
  • 37. ces-glacier-scaling-memo2009-01

    balance perturbations in climate change runs are typically on the order of 1 ma 1 so that over a period of a few or several decades, the ice surface may be lowered by several tens of metres. A lowering of that magnitude will start to affect the air temperature over the glacier and leads to an intensification of surface melting through the mass- balance–elevation feedback. Based on the preceding /media/ces/ces-glacier-scaling-memo2009-01.pdf
  • 38. Early work and an overview of measurements

    and an overview of measurements Secular variations of the climate of Iceland 1 Trausti Jónsson 23.1.2007 Evaluation of the history of climate in Iceland since the settlement has been ongoing for more than two hundred years. Hannes Finnsson, the bishop of Skálholt wrote /climatology/articles/nr/1138
  • 39. Early work and an overview of measurements

    and an overview of measurements Secular variations of the climate of Iceland 1 Trausti Jónsson 23.1.2007 Evaluation of the history of climate in Iceland since the settlement has been ongoing for more than two hundred years. Hannes Finnsson, the bishop of Skálholt wrote /climatology/articles/nr/1138/
  • 40. Supporting structures stopped most of an avalanche

    1 2 Supporting structures stopped most of an avalanche Avalanche above the health care centre of a town in north Iceland in 2012 27.4.2012 /about-imo/news/nr/2476

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