31 results were found for WA 0859 3970 0884 Anggaran Renovasi Rumah Type 21 Menjadi 2 Lantai Murah Wates Kulon Progo.

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. 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

  -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

• 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. 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

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

  drainage works, and land-cover and land-use change. Two other (sometimes indistinguishable) challenges to stationarity have been exter- nally forced, natural climate changes and low-frequency, internal variability (e.g., the Atlantic multidecadal oscillation) enhanced by the slow dynamics of the oceans and ice sheets (2, 3). Planners have tools to adjust their analyses for known human distur- bances /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 8. Lawrence_Deborah_CES_2010

  ) Green – Type 2: 34 – 66% (transitional) Blue – Type 3: < 33% (rainfall dominance) ⇒ Change towards increasing occurrence of autumn/winter peak flows in annual series Relative magnitude of rainfall- induced peak flows in annual series Ratio of Max (Aug – Feb) Max (all months) 1961 - 1990 2021-2050 ⇒Largest peak flow in some ’snowmelt’ areas is actually an autumn/winter rainfall flood Median /media/ces/Lawrence_Deborah_CES_2010.pdf

• 9. AnneFleig_May2010_CES

  Aug 1975 8 Apr−27 Jun 1993 NE Region DK1 SSEENNWSWW central CES conference, Oslo, Norway, 31 May - 2 June 2010 WT 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 − 2 Westerly SW NW Central Northerly NE Easterly SE Southerly Drought events are: • associated to several WTs; • mostly including different flow directions; • different events by different WTs; • only /media/ces/AnneFleig_May2010_CES.pdf

• 10. norsem_janutyte

  Fault plane solutions of the earthquakes in Nordland, Norway Ilma Janutyte(1), Jan Michalek(2), Conrad Lindholm(1), and Lars Ottemoller(2) (1) NORSAR, Kjeller, Norway, (2) University of Bergen, Bergen, Norway This study is a part of the ongoing NEONOR2 project which is carried out in Nordland, norther Norway. This work aims to define the fault plane solutions (FPS) of the earthquakes /media/norsem/norsem_janutyte.pdf