44 results were found for WA 0821 7001 0763 (FORTRESS) model pintu besi 2 daun Somolo - Molo Kabupaten Nias Sumatera Utara.

Results:

• 1. Kok_et_al._TFSC_published_2011

  All scenario groups identied 3–5 strategies of actions/milestones. Some (Sustainability Eventually) beforehand, others during (Fortress Europe) or after the exercise (Policy Rules and Economy First). Four strategies were identied in more than one group: 1. Institutions (EcF and PoR; fundamental to FoE and SuE) 2. Economy (EcF and PoR; noted as absent in SuE) 3. Climate-related (SuE and FoE /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 2. Milly_etal-2008-Stationarity-dead-Science

  drainage works, and land-cover and land-use change. Two other (sometimes indistinguishable) challenges to stationarity have been exter- nally forced, natural climate changes and low-frequency, internal variability (e.g., the Atlantic multidecadal oscillation) enhanced by the slow dynamics of the oceans and ice sheets (2, 3). Planners have tools to adjust their analyses for known human distur- bances /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 3. Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication

  Personality type differences between Ph.D. climate researchers and the general public: implications for effective communication C. Susan Weiler & Jason K. Keller & Christina Olex Received: 27 August 2009 /Accepted: 28 July 2011 / Published online: 2 September 2011 # The Author(s) 2011. This article is published with open access at Springerlink.com Abstract Effectively communicating the complexity /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 4. 2010_017

  of the volcanic zones in the south-western and the north-eastern part of the country due to the precipitation scaling. Figure 2. Mean annual number of days per year with snow covered ground for 1961– 1990 (Jónsdóttir, 2008). On watersheds where groundwater plays an important role, the above approximation leads to model parameters describing surface runoff and interflow that are very different from /media/ces/2010_017.pdf

• 5. Hare-2011-ParticipatoryModelling

  lcolumn ) 3Participatory Modelling in the Water Sector Copyright © 2011 John Wiley & Sons, Ltd and ERP Environment Env. Pol. Gov. (2011) DOI: 10.1002/eet 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 • participatory modelling purposes, • model type, • stakeholders involved, • timing /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 6. IPPC-2007-ar4_syr

  Assessment Re- port (AR4). Topic 1 summarises observed changes in climate and their ef- fects on natural and human systems, regardless of their causes, while Topic 2 assesses the causes of the observed changes. Topic 3 pre- sents projections of future climate change and related impacts un- der different scenarios. Topic 4 discusses adaptation and mitigation options over the next few decades /media/loftslag/IPPC-2007-ar4_syr.pdf

• 7. Journal_of_Hydrology_Veijalainen_etal

  calibration (Table 1). 3. Methods The main parts of the modelling are climate scenarios, transfer of the climate change to the hydrological model, hydrological mod- elling, frequency analysis and flood inundation analysis with hydraulic modelling (Fig. 2); these are presented in more detail in the following sections. Each part of the modelling chain contains uncertainties and by the end of the chain /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 8. 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

• 9. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  ORIGINAL ARTICLE Climate change adaptation in European river basins Patrick Huntjens • Claudia Pahl-Wostl • John Grin Received: 1 July 2008 / Accepted: 24 December 2009 / Published online: 2 February 2010  The Author(s) 2010. This article is published with open access at Springerlink.com Abstract This paper contains an assessment and stan- dardized comparative analysis of the current water man /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 10. Mo_Birger_CES_2010

  Introduction Outline Methodology 2 Electricity system model Area model Production capacities, 2020 3 Simulation results Hydropower Thermal production Energy balance CO2-emissions 4 Summary and concluding remarks Sintef Energy Research Quantitative system analysis 2 of 21 Introduction Electricity system model Simulation results Summary and concluding remarks Outline Methodology Outline Methodology /media/ces/Mo_Birger_CES_2010.pdf