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59 results were found for WA 0821 1305 0400 Spesialis Rumah Minimalis 2 Lantai Type 36/60 Berpengalaman Tapos Kota Depok.


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  • 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. 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
  • 3. VI_2021_008

    Tremv-ALERT: A new early warning system to detect volcanic tremor Bethany Vanderhoof Þórður Karlsson Yesim Cubuk Sabuncu Kristín Jónsdóttir VÍ 2021-008 Skýrsla Tremv-ALERT: A new early warning system to detect volcanic tremor VÍ 2021-008 ISSN 1670- 8261 Skýrsla + 354 522 60 00 vedur @vedur . is Veður st of a Íslands Búst aðaveg ur 7 – 9 108 Reyk j avík Bethany Vanderhoof Þórður Karlsson Yesim /media/vedurstofan-utgafa-2021/VI_2021_008.pdf
  • 4. 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
  • 5. 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
  • 6. VI_2019_009

    a71 a71 a71 a71 a71 a71 a71 a71 0 10 20 21 23 24 30 51 52 53 61 62 64 67 71 72 73 81 85 87 1 2 3 10 11 14 15 16 20 21 22 23 25 26 36 40 41 46 50 51 52 53 54 58 60 61 62 63 64 65 68 70 71 72 73 74 80 81 83 84 85 86 87 92 Present weather (Manual) Present weather ( Automatic ) Number of records a71 a71 a71 a71 5 10 15 20 5 10 15 20 Number of records Figure 16. Automatic records as a function of manual /media/vedurstofan-utgafa-2019/VI_2019_009.pdf
  • 7. 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
  • 8. IPPC-2007-ar4_syr

    such as tornadoes, hail, lightning and dust storms. There is no clear trend in the annual numbers of tropical cyclones. {WGI 3.2, 3.8, 4.4, 5.3, SPM} 2 Causes of change Topic 2 Causes of change 36 Causes of change This Topic considers both natural and anthropogenic drivers of climate change, including the chain from greenhouse gas (GHG) emissions to atmospheric concentrations to radiative /media/loftslag/IPPC-2007-ar4_syr.pdf
  • 9. 2010_005_

    Surface Air Temperature and Precipitation Trends for Iceland in the 21st Century Nikolai Nawri Halldór Björnsson VÍ 2010-005 Skýrsla Surface Air Temperature and Precipitation Trends for Iceland in the 21st Century VÍ 2010-005 ISSN 1670-8261 Skýrsla +354 522 60 00 +354 522 60 06 vedur@vedur.is Veðurstofa Íslands Bústaðavegur 9 150 Reykjavík Nikolai Nawri, Icelandic Meteorological Office Halldór /media/ces/2010_005_.pdf
  • 10. 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

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