88 results were found for WA 0821 7001 0763 (FORTRESS) pintu baja single Kaliwungu Kabupaten Kudus Jawa Tengah.

Results:

• 71. 2010_003rs

  ), further supporting that the transform motion has taken place mostly on a series of parallel north-trending faults, instead of a single large E-W fault. This type of faulting has been termed “bookshelf” faulting, as the blocks are thought to be slowly rotating counter clockwise when the northern block (i.e. the Hreppar micro-plate) moves left relative to the southern block (the Eurasian plate /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 72. VI_2014_005

  (PHYSICS=“arome”). Surface and soil processes are described by version 6 of the external single-layer coupled surface scheme SURFEX (SURFACE=“SURFEX”), consisting of special components for four different surface types: continental natural surfaces (including natural vegetation, bare soils, rocks, and permanent snow), town (including buildings, roads, and gardens), inland water (including lakes /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 73. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  versus warm or dry versus wet years) tend to average out more completely during a 30-year period than a single decade. The outline for the rest of this report is as follows. The GCM and RCM simulations used in the analysis are listed in Section 2. Section 3 describes how probabilistic climate change projections are derived by combining the results from the GCM and RCM simulations. In Section 4 /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

• 74. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  ´ttir & Gudmundsson 2006; Gudmundsson et al. 2007). The most accurate glacier map is the EMISAR DEM (B2 m accuracy in elevation for 5-m5-m spatial resolution and ca. 5-m positioning accuracy), pre- processed using a cross-calibration of single-pass inter- ferometeric C-band synthetic aperture radar data (Dall 2003) and further corrected and error estimated with available GCP and differential GPS /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 75. Keskitalo_et_al-MLG_and_adaptation_FINAL

  where they have not been part of EU projects. By using existing municipality co-operation networks and pooling funding, the KUUMA municipalities have been able to begin a preparation of a climate strategy that otherwise would have been beyond the means of small, single municipalities (Municipality of Mäntsälä, interview). 4.3. Adaptation in Sweden Issues of vulnerability and adaptation /media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf

• 76. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  Dissertation (working) title: Agency and Discourse in European Expansion: Who holds the reins in EU Policy North? Short description: Research will reveal the hidden power systems within the EU which seem to produce a European single projection of interests. My thesis documents the ways in which agency and dialogue construct the EU’s energy and environmental policies. I use the Arctic as a case /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 77. VI_2014_001

  - opment of multiple regression equations for estimating the index flood. For this reason, simple regression models were developed by combining several variables together into one single ex- planatory variable. Results were considerably improved compared to those obtained with one single variable such as the drainage area for instance, but the limited number of gauged sites can still be an obstacle /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 78. VI_2020_004

  of geological data, historical records and/or numerical model results (Mandeville et al., 2015). They can refer to a past eruption, to a specific hypothetical eruptive scenario or to a distribution of scenarios. If based on numerical results they can show the results from a single specific simulation (deterministic map) or from a multitude of scenarios. In the latter case the maps often represent /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 79. VI_arsskyrsla2020

  /media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf

• 80. VI_2015_009

  available in the studied region for developing a multiple linear regres- sion between index flood and catchment characteristics. Simple models were therefore devel- oped by combining several catchment characteristics into one single variable. Twelve variables, V , were defined: Variable no. 1: V = (A) Variable no. 2: V = (L) Variable no. 3: V = (A=L) Variable no. 4: V = (A=Z) Variable no. 5: V /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf