76 results were found for WA 0812 2782 5310 Pesan Pembuatan Interior Rumah Type 36/84 WIlayah Sukodono Sragen.

Results:

• 31. VI_2009_012

  .............................................................................................. 11  4  Recalculation of magnitudes and pgx-distance relations without near-source effect .. 12  5  Other predictor variables .............................................................................................. 19  6  Amplitude variations between stations and instrument type /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 32. VI_2015_009

  J600v berg 2.utg) were also used in this study. Table 1. Main characteristics of river basins used in this study. River Name Type Area Mean Percentage Mean annual Period / (km2) elevation glacier precipitation for Gauging (m a.s.l) (mm) streamflow station (1961-2014) data vhm59 Ytri-Rangá L 622 365 0 1564 1961–2014 vhm64 Ölfusá L+D+J+S 5687 480 12.2 2003 1950–2014 vhm66 Hvítá (Borgarfirði) L+J 1577 /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 33. 2010_017

  boundary flux between the unsaturated zone and the groundwater (Schulla & Jasper, 2007). Information on land use, soil type, elevation and other general properties of the watershed are given in static distributed grids while a number of parameters describing specific processes are adjusted to the properties of each watershed by comparison of modelled and measured discharge series. In this study /media/ces/2010_017.pdf

• 34. Perrels-CBA

  by level of the analytical process • Paradigm level: e.g. long term evolution in societal value systems and prioritization structures • scenario choices; delineation; (model type choice) • Conceptual level: understanding of the causal structure • Model (type) choice; model structure; data sources/needs • Model level: sufficiently adequate representation of the causal structure and orders /media/loftslag/Perrels-CBA.pdf

• 35. Workshop on Earthquakes in North Iceland

  of Akureyri Institute of Earth Sciences, University of Iceland KAUST, King Abdullah University of Science and Technology Húsavík Academic Center Icelandic Meteorological Office Earthquake Engineering Research Centre, University of Iceland Civil Protection Department, National Commisioner of the Icelandic Police Iceland Catastrophe Insurance Husavik Academic centre Ministry of the Interior /about-imo/news/nr/2701

• 36. VI_2015_007

  the report. 2 Study area and data 2.1 River basins The region under study is located in the East fjords and the surrounding area (Fig. 1). This region is characterised by a complex topography along the coast, Vatnajökull ice cap in the southwest and highlands in the interior. This leads to large precipitation and temperature gradients in the region (Crochet et al., 2007; Crochet & Jóhannesson, 2011). Eight /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 37. Pilot reports

  conditions encountered by an aircraft in flight. This information is usually relayed by radio to the nearest ground station. At a minimum the PIREP must contain a header, aircraft location, time, flight level, aircraft type and one other field. All significant weather encountered by an aircraft in flight, either to or from any Icelandic airport or airstrip, shall be reported to the Icelandic /weather/aviation/pirep/

• 38. Outline of the earthquake fault in Ölfus

  of the earthquake fault in Ölfus 30.5.2008 The map shows the location of the damaging earthquake that struck yesterday afternoon. Most movement took place along the fault shown in green. The black arrows denote right-lateral, strike-slip faulting. The same type /about-imo/news/nr/1312

• 39. norsem_janutyte

  package. From the recorded data we obtained nearly 120 FPS of the earthquakes and assigned them with the quality factors. We grouped the earthquakes into several groups according to their geographical locations, and investigated the obtained results in each group separately. The overall results in the study area show the dominating normal type of faulting and the N-S /media/norsem/norsem_janutyte.pdf

• 40. VI_2020_011_en

  and Surtsey would form a 3 cm thick deposit on Heimaey ....................... 36 Figure 15: Frequency of wind direction and wind speed ......................................................... 37 Figure 16: Probability of location of future vent opening based on the best fit line of the identified previous vents /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf