80 results were found for WA 0859 3970 0884 Jasa Interior Design Rumah Minimalis 1 Lantai Daerah Laweyan Solo.

Results:

• 1. vonKorff_etal-2010

  -y), which we call the design process, is the focus of much of this article. We would like to emphasize that design often develops, as in our view it should, through various feedback or iterative cycles. Figure 1 indicates this by the curved lines. Point x represents the situation that designers face when they begin their activities. This initial design context is usually characterized /media/loftslag/vonKorff_etal-2010.pdf

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

  6University of Washington, Seattle, WA 98195, USA. 7NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ 08540, USA. *Author for correspondence. E-mail: cmilly@usgs.gov. An uncertain future challenges water planners. Published by AAAS on July 12, 201 1 www.sciencemag.or g Downloaded from 1 FEBRUARY 2008 VOL 319 SCIENCE www.sciencemag.org574 POLICYFORUM combined with opera- tions /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 3. ESC-IASPEI-statement-LAquila-2012-1

  A Commission of the International Association of Seismology and Physics of the Earth’s Interior IASPEI Press release on the l’Aquila sentence The International Association of Seismology and Physics of the Earth Interior (IASPEI)1 The mission of IASPEI is to advance global seismological knowledge to mitigate the effects and minimize the victims of earthquakes. The trial in L'Aquila condemns some /media/vedurstofan/utgafa/hlidarefni/ESC-IASPEI-statement-LAquila-2012-1.pdf

• 4. Abstract_Impacts_of_Climate_Change_on_Stormwater_Systems_in_Reykjavik

  of decadal to multi-decadal variations related to natural climate variability, which may have counteracting effects on long-term trend detection, as the variations could be larger in magnitude than potential trends. The 1M5 Method is the primary method used in Iceland to find design precipitation intensity, based on the 1 day event with a 5 year return period (Elíasson, 1999). By updating /media/loftslag/Abstract_Impacts_of_Climate_Change_on_Stormwater_Systems_in_Reykjavik.pdf

• 5. 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

• 6. 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

• 7. Hare-2011-ParticipatoryModelling

  supports process monitoring and evaluation. Bots and van Daalen (2008) offer a similar framework to the one above (see Table 1). This too considers the timing of events and the participation mode, but also the type of model being produced and the purpose of the participatory modelling process. The framework is intended to support effective process design. The adapted framework used in this article /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 8. 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

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

  their audience. Climatic Change (2012) 112:233–242 DOI 10.1007/s10584-011-0205-7 C. S. Weiler (*) Office for Earth System Studies, Whitman College, Walla Walla, WA 99362, USA e-mail: weiler@whitman.edu J. K. Keller School of Earth and Environmental Sciences, Chapman University, Orange, CA 92866, USA C. Olex The Point, 121 Jewett Street, Newton, MA 02458, USA 1 Introduction Of all the applications /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 10. Hare_2-participation

  Visions & values wks Reference model Discuss Scenarios Framework 1 4 4 1 october november december january february Methodo. design september Options COURSE Process-oriented, input/output approach Steps ● Identify a logical series of stages as a framework ● Ask yourself at each stage ● What are the participatory goals? ● What stakeholders and how many of them (participation mode – Bots & van /media/loftslag/Hare_2-participation.pdf