35 results were found for WA 0821 1305 0400 Anggaran Biaya Pembuatan Rumah Type 21 2 Kamar Bogor Timur Kota Bogor.

Results:

• 1. 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

• 2. Kok_and_Veldkamp_editorial_ES-2011-4160

  and the environment: the importance of recognizing knowledge claims in transdisciplinary arenas. Ecology and Society 16(1): 21. [online] URL: http://www.ecologyandsociety.org/vol16/iss1/ art21/. Cash, D. W., W. Adger, F. Berkes, P. Garden, L. Lebel, P. Olsson, L. Pritchard, and O. Young. 2006. Scale and cross-scale dynamics: governance and information in a multilevel world. Ecology and Society 11(2): 8 /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 3. Isskyrsla_20101212

  Flugskýrsla TF-SIF 12. desember 2010 Flug nr. 117410.025 Áhöfn: Flugstjóri Hafsteinn Heiðarsson Flugmaður Jakob Ólafsson Flugmaður 2 / Þjálfunarfl. Yfirstýrimaður Auðunn F. Kristinsson Stýrimaður Gunnar Örn Arnarson Stýrimaður Stýrimaður Aðrir 9 farþegar, 4 til Akureyrar en 5 með allt flugið. Flugtími: Flugvöllur Hreyfing Flugtak Flugvöllur Lending /media/hafis/skyrslur_lhg/Isskyrsla_20101212.pdf

• 4. Kok_JGEC658_2009

  Change 19 (2009) 122–133 A R T I C L E I N F O Article history: Received 14 November 2007 Received in revised form 21 August 2008 Accepted 25 August 2008 Keywords: Fuzzy Cognitive Maps Scenario Participation Resilience Brazil A B S T R A C T The main drawback of the Story-and-Simulation approach is the weak link between qualitative and quantitative scenarios. A semi-quantitative tool, Fuzzy /media/loftslag/Kok_JGEC658_2009.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. VI_2021_008

  -time and detects signal characteristics similar to previously observed eruptions using a three-fold detection procedure based on: 1) an amplitude threshold; 2) the signal-to-noise ratio; and 3) an emergent ramp-like shape. Data from six Icelandic eruptions was used to assess and tune the module, which can provide 10–15 minutes of warning for Hekla up to over two hours of warning for some other /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

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

  These working hypotheses have been further developed into a methodology for evaluating the level of Adaptive and Integrated Water Management, which resulted in an ana- lytical framework for assessing regime characteristics, consisting of nine different dimensions of variables: 1. Agency 2. Awareness Raising & Education 3. Type of governance 4. Cooperation structures 5. Policy development /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 8. 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

• 9. 2005EO260001

  Dashed lines encompass the V-shaped zone of tephra deposition. (c) Oblique aerial view from west of the tephra plume at Grímsvötn on 2 November. Note the ashfall from the plume. (Photo by M. J. Roberts.) (d) Weather radar image at 0400 UTC on 2 November. The top portion shows its projection on an EW-vertical plane. The minimum detection height for Grímsvötn is seen at 6 km, and the plume extends /media/jar/myndsafn/2005EO260001.pdf

• 10. 2010_017

  m J M5 [C°] -3 obs. [C°] -4 nce 1 re 5. Comp 26); an int temperatu this system y gridded v picion abo -Jökulsá w similar dif han observ h elevation ces the effe months No ly only on high the tem n band wi refore be s onthly tem an Feb Ma .2 -3.1 -3. .3 -4.1 -3. .1 1.0 0.6 arison of m erpolation re is shown atic differe alues, see T ut the qual atershed; b ference wa ations for t gradient fo /media/ces/2010_017.pdf