70 results were found for WA 0821 7001 0763 (FORTRESS) pintu baja 2 pintu Medan Area Kota Medan Sumatera Utara.

Results:

• 21. News

  September 2012 as white dots, 20-21 October as red dots and 22-23 October as green dots (only M>2). The M5.6 event is marked as a black star. The blue circle shows the area of the cluster that was detected in the morning of 22 October. Tectonic faults are shown as black lines. News /about-imo/news/bigimg/2558

• 22. List of recent volcanic eruptions in Iceland

  1981 Krafla 2 eruptions 1981 Hekla 1980 Hekla 1980 Krafla 3 eruptions 1977 Krafla 2 eruptions 1975 Krafla 1973 subaquatic eruption 5 km south of Landeyjar coast 1973 Heimaey 1970 Hekla 1963-1967 Surtsey 1961 Askja 1947 Hekla 1938 Grímsvötn 1934 Grímsvötn 1933 Grímsvötn 1929 Askja 1927 Askja 1926 northeast of Eldey 1924 Askja 1923 Askja 1922 Askja 2 eruptions 1922 Grímsvötn 1921 Askja 1918 Katla /earthquakes-and-volcanism/articles/nr/1874

• 23. Hock_Regine_CES_2010rs

  in Scandinavia and Iceland • regional estimates • 2 glaciers (Storglaciären, Mårmaglaciären) Study area: Iceland, Scandinavia ~3,000 km2 ice Storglaciären (3.1 km2) Mårmaglaciären (3.9 km2) ~11,000 km2 ice Data Climate data, calibration period Monthly air temperature: ERA-40 reanalysis (0.5°×0.5°), 1958-2001 Monthly precipitation: Precipitation climatology VASClimO, 1951-2000, 0.5°×0.5° (Beck /media/ces/Hock_Regine_CES_2010rs.pdf

• 24. ces-glacier-scaling-memo2009-01

  vertical mass balance gradient averaged over the entire area of the glacier (a weighted average over the vertical range over which changes in the ice TóJ 2 5.12.2009 Memo surface elevation take place), and H is a scale for the ice thickness, defined as the gradient of volume changes to area changes, H = dV=dA, and assumed to be approximately constant over a substantial range in ice volume changes /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 25. 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

• 26. VI_2014_001

  @vedur . is Veður st of a Íslands Búst aðaveg ur 7 – 9 150 Reyk j avík Philippe Crochet, Icelandic Met Office Tinna Þórarinsdóttir, Icelandic Met Office   Contents 1 Introduction ................................................................................................ 7 2 Study area and data ..................................................................................... 8 /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 27. Machguth_Horst_CES_2010

  Horst Machguth, Andreas Ahlstrøhm, GEUS, Copenhagen Surface Mass Balance of the Greenland Ice Sheet in the Paakitsoq Area, Illulisat, West Greenland - Scenarios and Related Uncertainties 2 / 16 previous work A. P. Ahlstrøm Paakitsup Akuliarusersua (Paakitsoq) Thomsen & Olesen (1990) 2 / 16 previous work Paakitsup Akuliarusersua (Paakitsoq) Thomsen (1989) Thomsen & Olesen (1991) glacial /media/ces/Machguth_Horst_CES_2010.pdf

• 28. Increased glacial melt due to volcanic ash

  and sunny. The discharge far exceeded the mean and the volume that flowed in June, July and August was 1.4 km3 above average. This corresponds to 1.2 meters of ice melt over the whole drainage area of the glacier, but the total ice melt during the period was 2 meters. The figure also shows that spring melt in the highlands begins in April and May and glacier melt in June. Same is true for many /hydrology/articles/nr/2110

• 29. norsem_korja

  of earthquakes. Reference: [1] Korja, A. and Kosonen, E. M. (eds.) 2015. Seismotectonic framework and seismic source area models in Fennoscandia, Northern Europe. Univ. Helsinki, Instit. Seismology, Report S-63, 284 p. http://www.seismo.helsinki.fi/pdf/Seismotectonic_S63_Korja_Kosonen.pdf [2] Nørbech, T., Engsager, K., Jivall, L., Knudsen, O., Koivula, H., Lidberg, M., Ollikainen, M. & Weber, M., 2008 /media/norsem/norsem_korja.pdf

• 30. askja_minnisblad_ens

  ___________________________________________________ 2 therefore, the rims of the caldera are geologically a very young area. Such slopes are more unstable than slopes in older landscape. It is clear from geological evidence that rockslides similar to the one that fell in July 2014 have been released before from the rims of Askja, although people have not noticed them. Further rockslides in Askja should, therefore, be expected within /media/ofanflod/myndasafn/frodleikur/askja_minnisblad_ens.pdf