81 results were found for WA 0821 1305 0400 Design Interior Rumah Industrial 2 Lantai WIlayah Karangbahagia Kab Bekasi.

Results:

• 21. Rolf_Johnsen_(Region_Midt,_Dk)

  distribution, less rainfall in summer and more in winter. The precipitation pattern is expected to have a more dynamic cycle, with longer droughts and more intense rainfalls. As a result, groundwater models predict increases in groundwater levels of up to 2 metres in some areas (Van Roosmalen et al). Sea level will also rise. The precise increase is uncertain but models show increases of up /media/loftslag/Rolf_Johnsen_(Region_Midt,_Dk).pdf

• 22. 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

• 23. CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction

  in sea surface level in the North Sea/Baltic Sea system whereas changes in sea surface level coursed by tides is small with a range of less than 0.5 m. Figur 1. Horsens Fjord catchment. WFD main catchment area is 794 km2 NONAM Risk Assessment and Stakeholder Investment. Multidisciplinary Workshop in Reykjavík 26 – 27 August 2010 2 Physical features and ecosystem The fjord landscape /media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf

• 24. Case_A___Horsens_Fjord

  in sea surface level in the North Sea/Baltic Sea system whereas changes in sea surface level coursed by tides is small with a range of less than 0.5 m. Figur 1. Horsens Fjord catchment. WFD main catchment area is 794 km2 NONAM Risk Assessment and Stakeholder Investment. Multidisciplinary Workshop in Reykjavík 26 – 27 August 2010 2 Physical features and ecosystem The fjord landscape /media/loftslag/Case_A___Horsens_Fjord.pdf

• 25. Linnet_Ulfar_CES_2010

  concern Regular use of flow series •Every autumn reservoir content is forecasted one year into the future •When designing or reviewing design of new units. Reservoir size and installed capacity are based on reservoir inflow. •For long term contracts a due diligence study is performed •Larger research projects. For instance connecting Iceland to Europe with a submarine power cable. Expected inflow /media/ces/Linnet_Ulfar_CES_2010.pdf

• 26. Hare_2-participation

  aceptance of solution Creating conditions for implementation of solution Implementation of solution Monitoring & Evaluation Knowledge elicitation; system identification Poor functioning system Well functioning system 5 Lectures – Creating awareness Forum 1 15.9.04 Forum 2 3.11.04 6 Cognitive mapping Knowledge Elicitation Forum 1 15.9.04 Forum 2 3.11.04 Interviews Jan/Feb 05 7 Forum 1 /media/loftslag/Hare_2-participation.pdf

• 27. Keskitalo_et_al-MLG_and_adaptation_FINAL

  Connecting multiple levels of governance for adaptation to climate change in advanced industrial states E. Carina H. KESKITALO1 (Carina.Keskitalo@geography.umu.se) Sirkku Juhola 1 (Sirkku.Juhola@tkk.fi) Lisa Westerhoff 1 (lisa.westerhoff@gmail.com) Forthcoming in: Connective Capacities in Water Governance (eds. J. Edelenbos, N. Bressers and P. Scholten). Ashgate, London. 1 /media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf

• 28. VI_2015_007

  stations. Next, the method is developed with simulated streamflow series obtained with WaSiM on selected catchments, as described above. The report is organized as follows. Section 2 presents the study area and data. Section 3 describes the methodology. Section 4 presents the results of the proposed approach for estimating design floods at ungauged catchments. Finally, Section 5 concludes /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 29. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  –2°C, relative to the pre-industrial level, in the near future and by approximately 2–3°C towards the end of the century. The largest temperature increase is expected during winter. Equivalent projections for the mean annual precipitation show a small increase in the short term, becoming more pronounced in the long term. The strongest positive precipitation response is seen during winter, whereas /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 30. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

  296 Public Choice (2010) 143: 293–301 2 The commons The literature on the commons, or what is more technically defined as common-pool re- sources (CPRs), should be viewed initially from its place in the larger literature on dilem- mas of collective action. Since the foundational work of H. Scott Gordon (1954) on the com- mons, and Mancur Olson (1965) on collective action more broadly, the behavioral /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf