77 results were found for WA 0821 1305 0400 Pembuat Lantai Vynil Sticker Rumah Green Building Di Sukaraja Kab Bogor.

Results:

• 41. Risk Assessment and Stakeholder Involvement

  The workshop The workshop aims at the strengthening links and exchange information among Nordic researchers and practitioners in adaptive management related to climate change. The workshop concentrates on three topics: What is the difference between adaptation and adaptive management? Participatory planning process - group model building Uncertainty and risk assessment For all topics /nonam/workshop/

• 42. ces_cg_flyer

  information, contact: Erik Kjellström (erik.kjellstrom@smhi.se) 2) Probabilistic climate change scenarios building on the CMIP3 AOGCMs and the ENSEMBLES/CES RCMs are developed within the CES project. The example above shows the probability (%) that decadal mean precipitation will exceed the mean for 1971-2000 based on CMIP3 AOGCMs. 3) Interpretation of regional climate scenarios, to approximately 1 /media/ces/ces_cg_flyer.pdf

• 43. Horsens_breakout_12August

  1 Horsens case – Break out groups Jens Christian Refsgaard and Hans Jørgen Henriksen, GEUS The Horsens case deals with climate change adaptation of water issues in the Horsens area. The aim of the group work is to work actively with the four topics covered during lecturing (scenario building, stakeholder involvement; risk perception/acceptability and uncertainty) in a specific case /media/loftslag/Horsens_breakout_12August.pdf

• 44. Kok_JGEC658_2009

  /media/loftslag/Kok_JGEC658_2009.pdf

• 45. VI_2014_001

  at each site i with the same method used to estimate qR(D;T ), but instead of pooling AMF series for a given duration D from different sites, the estimation is made individually for each site i by pooling AMF series for different durations D (see Crochet, 2012c). The index flood µi(D), is modeled at each site i as a continuous function of D, as follows: µi(D) = µi 1+(D=Di)li ; (5) where µi, Di /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 46. VI_2021_008

  in Figure 8a are colored green, while the three to the NE plotted in Figure 8b are colored yellow. Table 2. Table of the visually picked arrival times of the Hekla 2000 eruption tremor to stations WSW of the volcano (hau, sau, kri, grv) and NE of the volcano (skr, ren, gil). Tremor velocities are with respect to the previous station. Bearing from Hekla Station Name Distance from /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 47. Lorenzoni_Pidgeon_2006

  and promoter of the Protocol and the UK has taken up a leading role on the issue, especially during its presidency of the EU and the G8 in 2005. The USA, on the other hand, as the greatest emitter of greenhouse gases, withdrew from the Kyoto Protocol in 2001 and has based its ∗Preasent address: School of Psychology, Cardiff University, Tower Building, Park Place, Cardiff CF 10 3AT, UK, E-mail /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 48. Avalanche notices on the web - an improved map

  Medium Avalanche Could bury and destroy a car, damage a truck, destroy a small building or break a few trees Snow avalanche could traverse flat terrain (consideralbly below 30°) over distances of less than 50m Size 4 Large Avalanche could bury and destroy a railway car, large trucks, several buildings or a piece of forest Snow avalanche traverses flat terrain (considerably below 30°) over /about-imo/news/nr/2838

• 49. Supporting structures stopped most of an avalanche

  below the structures (see the map below). The supporting structures clearly prevented the release of a much larger avalanche. Map of Tvísteinahlíð showing the outline of the avalanche that was released on 19 March 2012 (thick, red curve). The narrow curves show outlines of historical avalances. The health care centre is the large H-shaped building close to the hillside. The rows of supporting /about-imo/news/nr/2476

• 50. Workshop on Earthquakes in North Iceland

  ), the 1963 Skagafjörður earthquake (M7.0), and the 1976 Kópasker earthquake (M6.3). Recent research results show that stress is steadily building up in the Tjörnes Fracture Zone and that the area may be due for another large earthquake. Workshop In light of the new activity and newly published research results, a workshop will be held focussing on earthquakes in North Iceland. The workshop has /about-imo/news/nr/2701