46 results were found for WA 0821 7001 0763 (FORTRESS) Model Pintu Rumah 1 Pintu Terbaru Teramang Jaya Mukomuko.

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

  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. 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

• 4. 2010_017

  ............................................................................................................................. 24 7 1 Abstract The WaSiM model is used for hydrological modelling at the Icelandic Meteorological Office. The model application has been improved from former use by: i) improving the representation of groundwater by activating the model’s groundwater module; ii) improving the representation of seasonal changes in the Hamon evapotranspiration /media/ces/2010_017.pdf

• 5. 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

• 6. 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

• 7. 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

• 8. 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

• 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. Linnet_Ulfar_CES_2010

  from 1950 to 2008 have been simulated using a hydrological model •These series were used to determine generation capacity and for new development •Since the start of CWE, CE, CES the use of these historical series has been questioned and is now abandoned •Currently 2010 series are being used for operational planning and 2010 and 2025 series for design •New series have been made for 2010 /media/ces/Linnet_Ulfar_CES_2010.pdf