62 results were found for WA 0821 7001 0763 (MEVVAH) White Wall Panel Marmer Ile Ape Kabupaten Lembata Nusa Tenggara Timur.

Results:

• 31. Eyjafjallajokull_status_2010-06-10_IES_IMO

  detection system, web-based ash reports from the public and research expedition of the IES to the summit on 3/6-2010. Eruption plume: Height (a.s.l.): No information Heading: SW-wind today, turning towards NW-wind tonight. Colour: White (when last seen late on 7-8 June). Tephra fallout: No informaiton Lightning: None were measured on the UK Met Office's system but 32 lightnings were /media/jar/Eyjafjallajokull_status_2010-06-10_IES_IMO.pdf

• 32. IMO_AnnualReport2014

  which descended into the caldera lake (Lake Öskjuvatn). The slide was released from the southeastern caldera wall, triggering a tsunami in the lake that washed up on the lakeshores all around the lake, reaching up to 20–30 m elevation above the water level. The wave travelled farthest around 400 m (horizontally) into the flatland SE of the crater Víti. Fortunately, the rockslide occurred /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 33. A glimpse into the field

  opportunity. Ármann Höskuldsson, IES, sent an illustrated account of the situation: The fissure All the active part of the fissure, at noon 12 September 2014. Photo: Ármann Höskuldsson. The lava is still advancing in the riverbed of Jökulsá á Fjöllum. A narrow flow with heavy current is between the lava and the eastern wall of the riverbed. Occasionally, small steam explosives occur /about-imo/news/nr/2985

• 34. A glimpse into the field

  opportunity. Ármann Höskuldsson, IES, sent an illustrated account of the situation: The fissure All the active part of the fissure, at noon 12 September 2014. Photo: Ármann Höskuldsson. The lava is still advancing in the riverbed of Jökulsá á Fjöllum. A narrow flow with heavy current is between the lava and the eastern wall of the riverbed. Occasionally, small steam explosives occur /about-imo/news/nr/2985/

• 35. Journal_of_Hydrology_Veijalainen_etal

  The hydrological simulations were performed with the Wa- tershed Simulation and Forecasting System (WSFS) developed and operated in the Finnish Environment Institute (Vehviläinen et al., 2005). The WSFS is used in Finland for operational hydrolog- ical forecasting and flood warnings (www.environment.fi/water- forecast/), regulation planning and research purposes (Vehviläinen and Huttunen, 1997 /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 36. Bárðarbunga - decay of seismic activity

  the cumulative seismic moment release per week (blue dots), i.e. the sum of the moment of all earthquakes in the respective week, in the left panel for the caldera and in the right panel for the dyke intrusion. The red line marks the onset of the eruption and the zero point is the beginning of the earthquake swarm on 16 August 2014. The last data point shows the current week (might still rise). Note /earthquakes-and-volcanism/articles/nr/3083

• 37. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  at Springerlink.com Abstract We propose a generic framework to characterize climate change adaptation uncertainty according to three dimensions: level, source and nature. Our framework is different, and in this respect more comprehensive, than the present UN Intergovernmental Panel on Climate Change (IPCC) approach and could be used to address concerns that the IPCC approach is oversimplified. We have studied /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 38. Dyngjujökull station

  A seismometer has been in operation by the IMO at the site since the autumn of 2014 and the main purpose of the new station is to monitor the weather conditions at this important station in the network amongst the volcanoes of Vatnajökull (Bárðarbunga, Grímsvötn, Hamarinn and Kverkfjöll). The station is powered by a wind generator and a solar panel (during summer). Location information is as follows /about-imo/news/dyngjujokull-1

• 39. Monitoring flow

  electronic registration equipment, pressure sensor to measure the water level, sensors for the conductivity and temperature in the water, solar-panel which provides energy for the station, a telephone and a modem for the transfer of data. An alarm goes off when conductivity or the water level reaches a given limit and alerts Neyðarlínan (the Emergency Watch), bringing in specialists who decide /hydrology/flow/

• 40. Acquiring knowledge for our future

  Acquiring knowledge for our future 10.4.2008 In Budapest, Hungary, the Intergovernmental Panel on Climate Change are holding their 28th session. At this meeting, IPCC will decide how to allocate the financial award received when /about-imo/news/nr/1277