48 results were found for WA 0812 2782 5310 Biaya Renovasi Rumah Type 30/60 2 Lantai Terpercaya Pringapus Kab Semarang.

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. Alam_Ashraful_CES_2010

  Short distance transportation Long distance r g y i n p u t o x i d e E m i s M W h - 1 8 4 - M5 (-20%) M6 (-30%) Energy wood in power plant Timber in pulp and saw mill transportation Chipping s i o n s K g C O 2 (b) Norway spruce: Myrtillus type 10 l a r e a ( m 2 h a - 1 ) Basal area just before thinning Remaining basal Thinning threshold Energy wood thinning 8 9 B a s a l /media/ces/Alam_Ashraful_CES_2010.pdf

• 3. 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

• 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. Lawrence_Deborah_CES_2010

  -2050 30-year flood XX Flood frequency estimation applied to annual maximum flood series % change in 200-year flood Projected change in 200-yr. flood between 1961-1990 and 2021-2050 Change (%) 90th percentile of 150 models Median of 150 models Change (%) Range of uncertainty in projections Median of 150 models Change (%) Range (%) Range 10 to 90% Downscaling method 0 10 20 30 40 50 60 70 80 90 /media/ces/Lawrence_Deborah_CES_2010.pdf

• 6. 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

• 7. 2010_005_

  on the reduced IPCC ensemble, it is likely that TP will increase at a rate of about 1% of the 1961–90 average per decade throughout the 21st Century, with somewhat lower trends over the ocean than over the land area. 22 !30 !25 !20 !%5 !%0 !5 0 &0 &2 &4 && &( )0 IPCC Mean SAT (1961!90) !20 !%5 !%0 !5 0 5 %0 !30 !25 !20 !%5 !%0 !5 0 &0 &2 &4 && &( )0 IPCC Mean SAT Change (1961!90 to 2021!50) 0 0+5 /media/ces/2010_005_.pdf

• 8. 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

• 9. Bardarbunga_kafli20140825

  characteristics: Type of products: Airborne tephra, water transported tephra Volcanic Explosivity Index Max: VEI 4; most freq: VEI 3-4; min: VEI 0 Column heights: No information Duration of eruptions: Weeks to months Bulk volume tephra (km3): Max: no information, aver: 0.1, min: no information Fallout beyond 1000 km: No information Tephra <63µm at 30 km No information Bulk volume lava /media/jar/Bardarbunga_kafli20140825.pdf

• 10. AnneFleig_May2010_CES

  drought-supporting WTs over previous n days (n = 1, 15, 30, 45, 60, 90, 120, ... 330). Determination of the period of influence: dreg 90 45 little groundwater45 45 CES conference, Oslo, Norway, 31 May - 2 June 2010 210 60 45 60 highly productive aquifers moderately productive aquifers}90 210 60 60 Anne K. Fleig et al. “Regional hydrological droughts and weather types in north-western Europe /media/ces/AnneFleig_May2010_CES.pdf