47 results were found for WA 0821 7001 0763 (FORTRESS) Pintu Plus Handle Pintu Rumah Tanah Sepenggal Lintas Bungo.

Results:

• 41. VI_2009_006_tt

  than can be expected to originate from the cauldrons, three to four times the wa- ter equivalent of the accumulation of snow over the watershed of the cauldrons. It has been estimated that flow from the cauldrons, in addition to the jökulhlaups, could be 2–5 m3 s 1 at maximum (Vatnaskil, 2005). It is possible that part of the sulfate-rich groundwater from the glacier comes from the cauldrons /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 42. Publications

  /CWE workshop. Reykjavík, Iceland. Oct 9. [Presentation] Bergström, S. (2003). Klarar våra dimensioneringsregler dagens och framtidens klimatvariationer? (Can our design rules handle the climate variations of today and tomorrow?). Invited breakfast-lecture, WSP. Stockholm. March 4. Bergström, S. (2003). Klimatet och vattnet (Climate and water). Invited lecture on climate and hydropower at Svensk /climatology/research/ce/publications/

• 43. vonKorff_etal-2010

  the préfet, on how to set up a participatory process for a specific policy decision. Mazri has tested his approach in a risk management context but emphasizes its applicability in other areas. The approach is a design process of five phases, including advice on how the designer should proceed in each phase plus various models for illustration. To develop this design process, Mazri extensively reviewed /media/loftslag/vonKorff_etal-2010.pdf

• 44. 2010_003rs

  /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 45. 2010_012rs

  not handle events smaller than M3 very well; they usually trigger only one or two stations and the estimates obtained are rather scattered. The long-period M2-3 events constantly occurring in the Katla volcano in southern Iceland (shown with a blue star in Figure 1) are also problematic. They have very different characteristics from regular tectonic events in Iceland and return very high τmax values /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 46. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 47. ces-oslo2010_proceedings

  anomalies of the WTs during the periods leading up to the five most severe droughts as compared to the average frequency of a given WT for the same period of the year over the entire data record. A period equal to dreg preceding the drought plus the 20 first days of the drought was used. All WTs with a net positive frequency anomaly over the five events were considered to be associated /media/ces/ces-oslo2010_proceedings.pdf