62 results were found for WA 0821 1305 0400 RAB Pemasangan Plafon Model Eropa Bogor Barat Kota Bogor.

Results:

• 31. Articles

  ágúst 2014. Höfundur Bogi Brynjar Björnsson. Of interest - Bárðarbunga Reduction of the accesscontrolled area around Holuhraun lava field END OF ERUPTION declaredby the Scientific Board Location map (detailed)around the new lava field Bárðarbunga earthquakes3D interactive model /earthquakes-and-volcanism/articles/bigimg/2948

• 32. Articles

  )around the new lava field Bárðarbunga earthquakes3D interactive model Thickness and volumeestimate from January 1st Comparing historic sizes of lavafields: AD 934 and 1783 Gas dispersion model Preliminary flood risk assessmentfor Jökulsá á Fjöllum Web cameras of Míla Web cameras of M&T Related topics /earthquakes-and-volcanism/articles/bigimg/3158

• 33. Of interest - Bárðarbunga

  earthquakes3D interactive model Thickness and volumeestimate from January 1st Comparing historic sizes of lavafields: AD 934 and 1783 Gas dispersion model Preliminary flood risk assessmentfor Jökulsá á Fjöllum Web cameras of Míla Web cameras of M&T Related topics Instructions on using earthquake pages /earthquakes-and-volcanism/articles/bigimg/

• 34. Articles

  Articles © Icelandic Meteorological Office An example from the web. Temperature forecast by the HARMONIE model /weather/articles/bigimg/3232

• 35. norsem_asdis

  the first tomographic model of Eyjafjallajökull volcano, south Iceland, using ambient noise tomography. The data were collected on a dense network of temporary and SIL seismometers prior to and during the 2010 eruption. Cross-correlations between stations enabled us to construct phase-velocity dispersion curves and create phase-velocity maps, for periods between 1.6-6.5 s /media/norsem/norsem_asdis.pdf

• 36. Refsgaard_etal-2007-Uncertainty-EMS

  uncertainty), Monte Carlo analysis, multiple model simulation, NUSAP, quality assurance, scenario analysis, sensitivity analysis, stakeholder involvement and uncertainty matrix. The applicability of these methods has been mapped according to purpose of application, stage of the modelling process and source and type of uncertainty addressed. It is concluded that uncertainty assessment is not just /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 37. Paper-Olafur-Rognvaldsson_92

  for Meteorological Research, Reykjavík, Iceland 5Bergen School of Meteorology, Geophysical Insitute, University of Bergen, Norway †Corresponding author: or@belgingur.is, Orkugarður, Grensásvegur 9, 108 Reykjavík ABSTRACT Atmospheric flow over Iceland has been simulated for the period Jan- uary 1961 to July 2006, using the mesoscale MM5 model driven by initial and boundary data from the ECMWF. Firstly /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 38. Machguth_Horst_CES_2010

  experiments with different RCM’s • explore RCM biases • apply a different mass balance model data 2 RCM’s • HIRHAM4, Scenario A1B, 25 km, 1950-2100, Greenland • RCAO, Scenario A1B, 50 km, 1960-2100, Pan-Arctic 4 Weather Stations (Ta, Sin) • GC-Net Swiss Camp: 1150 m a.s.l. (1995 – 2006) • GC-Net Crawford: 2020 m a.s.l. (1995 – 2006) • Asiaq Station 437: 300 m a.s.l. (1983 – 2006) • DMI Illulisat /media/ces/Machguth_Horst_CES_2010.pdf

• 39. Hock_Regine_CES_2010rs

  Step 1: Temperature-index mass- balance model Monthly temperature Monthly precipitation Step 1: Temperature-index mass- balance model Step 2: Extrapolation of model parameters to all glaciers in Iceland and Scandinavia • Monthly temperature • Monthly precipitation • Gridded climate variables Methodology Step 1: Temperature-index mass- balance model • Monthly temperature • Monthly /media/ces/Hock_Regine_CES_2010rs.pdf

• 40. Refsgaard_2-uncertainty

  sources Consultant # 1 Consultant # 2 Consultant # 4 Consultant # 5 Consultant # 3 Vulnerable areas Very vulnerable Vulnerable Less vulnerable Well protected Prediction uncertainty due to - data interpretations - model parameter values - models (process equations) - problem framing The Water Management Process and the Hydrological Modelling Process  Uncertainty assessments influence /media/loftslag/Refsgaard_2-uncertainty.pdf