79 results were found for WA 0812 2782 5310 Anggaran Rehab Rumah Minimalis Type 36/72 Berpengalaman Tawangsari Sukoharjo.

Results:

• 61. Group5-Participation_stages

  1 Stakeholders involvement – Participation stages Participation stage Duration stakeholders Participatory level Type of knowledge Knowledge elicitation 1 Problem identification (Stakeholder analysis) 2 months  Horsten municipality (Competent authority) n.a 2 Information provision 2 months  Horsten municipality  Policy maker  Insurers  Neighbouring municipality /media/loftslag/Group5-Participation_stages.pdf

• 62. Alam_Ashraful_CES_2010

  • Methodology • Key findings • Conclusions 2 Forestry in Finland 1. Land area distribution 2. Species distribution Total Forestry land 26.3 mill. ha 3. Growing stocks, increment and drain 4. Site type distribution Source: Finnish Forest Research Institute, 2008 3 Forest management Final felling Timber Energy biomass Thinning Timber Pre-commercial or energy biomass thinning Regeneration Regeneration 4 /media/ces/Alam_Ashraful_CES_2010.pdf

• 63. Lawrence_Deborah_CES_2010

  1 10 100 1000 Return period (years) P e a k d a i l y d i s c h a r g e ( m 3 / s ) 1961-1990 Gumbel 2021-2050 Gumbel 2021 - 2050 annual maxima 1961 - 1990 annual maxima X X 35% increase in 200-year flood Model uncertainty Seasonal analysis - Rainfall-induced peak flows in annual maximum series 1961 - 1990 2021-2050 Red – Type 1: > 67% of annual maximum in mar-july (snowmelt dominance /media/ces/Lawrence_Deborah_CES_2010.pdf

• 64. Kok_2-scenarios-lecture-2

  extreem events C6; qual nat. systems C7; policies C8; price of resources C9; other sectors C10; industry C11; inrastructure Crimea - Ukraine Manaus - Brazil From FCM to model input FCM – strong points • Easy to develop and apply. The approach is highly intuitive, it can quickly be explained and applied to any new situation. • High level of integration. A FCM can contain any type of information /media/loftslag/Kok_2-scenarios-lecture-2.pdf

• 65. CES_D2.4_task1

  %, respectively. For the best-estimate distribution representing the year 2010, the probability of warm Decembers has increased to 72% and the probability of very warm Decembers to 26%1; conversely the probabilities of cold and very cold Decembers have been reduced. A part of these changes is already visible in the observed distribution for 1961-2008. 1 /media/ces/CES_D2.4_task1.pdf

• 66. 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

• 67. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  and the organising of the participatory process. 2. BNs with stakeholder involvement and the NeWater context 2.1. Bayesian networks A Bayesian belief network, also called a BN, is a type of decision support system based on probability theory which implements Bayes’ rule of probability. This rule shows mathematically how existing beliefs can be modified with the input of new evidence. BNs organise /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 68. 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

• 69. ces-glacier-scaling-memo2009-01

  in km2 and km3, respectively, and c = 0:036, g = 1:36 for the valley glaciers. Figure 2 shows the same five Icelandic ice caps and the same regression lines together with volume–area data for eight ice caps and glaciers on Svalbard and in Scandinavia and the much larger ice sheets of Greenland and Antarctica. Figures 1 and 2 show that reasonable approximations for the ice volume stored in glaciers /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 70. Fractures in Svínafellsheiði and a potential rockslide on Svínafellsjökull

  cap and, in 2007, a rock avalanche fell on the Morsárjökull outlet glacier in southern Vatnajökull ice cap. Rockslides and rock avalanches on glaciers may break up the surface of the glacier, thereby adding ice to the moving material. In addition, the slide may sweep water from glacial lagoons on its way, creating a fast-flowing slurry of rock, ice, water and even air. Debris flows of this type /about-imo/news/fractures-in-svinafellsheidi-and-a-potential-rockslide-on-svinafellsjokull