65 results were found for WA 0859 3970 0884 RAB Pembuatan Kamar Set Mewah Ukir Jepara Di Bulu Sukoharjo.

Results:

• 11. VI_2014_005

  of the HAR- MONIE model have a relaxation zone of 10 grid points, wherein the coarse-resolution outer data from the host model is blended with the high-resolution data within the dependent model domain. At the upper boundary, defined as the 10-hPa isobaric surface, vertical velocity is set to zero. The model is run in upper-air and surface data assimilation mode. The atmospheric analysis is handled /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 12. VI_2020_011_en

  Veðurstofa Íslands 2 Almannavarnadeild Ríkislögreglustjóra 3 Jarðvísindastofnun Háskólans 4 Istituto Nazionale di Geofisica e Vulcanologia (INGV), Bologna 5 Istituto Nazionale di Geofisica e Vulcanologia (INGV), Pisa 6 Jarðvísindadeild Háskóla Íslands 7 Agricultural University of Iceland 8 Consultant Skýrsla nr. Dags. ISSN Opin Lokuð VÍ 2020-011 Desember 2020 1670-8261 Skilmálar: Heiti skýrslu /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 13. Keskitalo_et_al-MLG_and_adaptation_FINAL

  in the discussion of national adaptation strategies (cf. Swartz et al. 2009; Biesbroek et al. 2010). Arguing that until then these developments had ‘only been assessed in a superficial manner’ (Biesbroek et al. 2010, p. 441), one recent set of studies has analysed the development and content of national adaptation strategies to draw lessons on the emergence of adaptation (Swart et al 2009 /media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf

• 14. VI_2014_001

  for the lack of temporal data by spatial data, taken within a region with similar flood behaviour and transfer information from gauged to ungauged sites. The underlying assumption is that flood data within a homogeneous region is drawn from the same frequency distribution, apart from a scaling factor. The method involves two major steps, i) the identification of a set of hydrologically /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 15. Refsgaard_etal-2007-Uncertainty-EMS

  Uncertainty assessment of model simulations is therefore important, when models are used to support water management decisions (Beven and Binley, 1992; Beven, 2002; Pahl-Wostl, 2002; Jakeman and Letcher, 2003; Refsgaard and Henriksen, 2004; Pahl-Wostl, 2007; Vandenberghe et al., 2007). Model un- certainty is in practice often done as an ‘end of pipe’ analysis that is carried out after model set-up /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 16. Grimsvotn_status_2011-05-30_IES_IMO

  Since Thursday the tremor had been intermittent. Today, Monday 30 May, it has been confirmed by the participants of Iceland Glaciological Society's spring expedition that the eruption has ended. The end of the Grímsvötn eruption is set to 7 UTC Saturday morning 28 May 2011. /media/jar/Grimsvotn_status_2011-05-30_IES_IMO.pdf

• 17. 2013_001_Nawri_et_al

  /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 18. VI_2009_006_tt

  of the subglacial seal at the beginning of the 1996 jökulhlaup and concluded that the high water level reached before the on- set of the 1996 flood could be explained with the traditional theories of Röthlisberger (1972) and Nye (1976) but he did not address the rapid discharge increase following the breaking of the seal. Flowers et al. (2004) concluded that a model fundamentally different from /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 19. VI_2016_006_rs

  in a collaboration between the Austrian engineering company Ingenieurbüro Illmer Daniel e.U. (DI), Efla consulting engineers and the Icelandic Meteorological Office (IMO). Daniel Illmer carried out the analysis of landslide protection measures, Jón Kristinn Helgason, Tómas Jóhannesson and Eiríkur Gíslason wrote sections about the geographical setting, the land- slide history and the assessment /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 20. Adalgeirsdottir-etal-tc-5-961-2011

  the set- tlement, glaciers were smaller than at present. They started to advance in the 13th century at the onset of the Little Ice Age that lasted until late 19th century when most glaciers in Iceland reached their maximum extent. In the 20th century, the climate was significantly warmer than during the Little Ice Age, with higher temperatures in the period 1930–1945 and again at the end /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf