34 results were found for WA 0859 3970 0884Biaya Pembangunan Renovasi Rumah Type 90 1 Lantai Murah Surakarta.

Results:

• 1. 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

• 2. 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

• 3. Lawrence_Deborah_CES_2010

  1 10 100 1000 Return period (years) P e a k d a i l y d i s c h a r g e ( m 3 / s ) 1961-1990 Gumbel 2021-2050 Gumbel 2021 - 2050 annual maxima 1961 - 1990 annual maxima X X 35% increase in 200-year flood Model uncertainty Seasonal analysis - Rainfall-induced peak flows in annual maximum series 1961 - 1990 2021-2050 Red – Type 1: > 67% of annual maximum in mar-july (snowmelt dominance /media/ces/Lawrence_Deborah_CES_2010.pdf

• 4. 2010_005_

  is reduced. 3.2 Total Precipitation As with surface air temperature (SAT), total precipitation (TP) depends on surface type and terrain elevation (see Fig. 9). Similarly to SAT, the terrain of Iceland only induces a weak wave pattern in the larger-scale northeast to southwest gradient in the GCM ensemble mean field of TP during the 1961–90 control period, resulting in about 0.5 mm day 1 lower mean /media/ces/2010_005_.pdf

• 5. IPPC-2007-ar4_syr

  the respective WG reports. Unless otherwise stated, numerical ranges given in square brackets in this report indicate 90% uncertainty intervals (i.e. there is an estimated 5% likelihood that the value could be above the range given in square brackets and 5% likelihood that the value could be below that range). Uncertainty intervals are not necessarily symmetric around the best estimate. 1 Observed changes /media/loftslag/IPPC-2007-ar4_syr.pdf

• 6. BIGJ_windrose_2005-2014

  Wind rose BIGJ 2005 − 2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 1 2 3 4 5 6 7 Frequency of wind direction (%) Aerodrome Total observations: 1324 Calm: 2.6% Variable winds: 0.23% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 0 45 90 135 180 225 270 315 360 N E S /media/vedur/BIGJ_windrose_2005-2014.pdf

• 7. VI_2009_006_tt

  was therefore formed by ice lifting and deformation induced by subglacial water pressures higher than ice overburden pressure. The discharge data and the derived size of the subglacial flood path, as indicated by the volume of water stored subglacially, indicates a development towards more efficient subglacial flow over the course of the jökulhlaup. Thus, a discharge in the iii range 80–90 m3 s 1 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 8. BIBD_windrose_2005-2014

  W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 36 2 69 4 138 2 187 3 151 2 106 7 83 1 58 1 36 0 20 3 17 6 14 5 14 9 11 0 10 6 13 0 16 7 29 8 55 2 73 0 95 6 140 7 98 9 41 9 20 2 17 7 8 1 6 4 4 8 3 7 5 7 4 4 4 5 7 3 9 2 18 5 Wind rose BIBD January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 /media/vedur/BIBD_windrose_2005-2014.pdf

• 9. 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

• 10. BIVO_windrose_2005-2014

  S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 26 8 27 9 44 9 36 0 111 1 173 2 39 3 24 9 20 7 9 0 2 9 4 7 1 0 1 4 3 3 1 6 2 6 3 5 6 8 10 1 27 3 39 0 86 7 209 6 71 4 25 7 21 5 8 2 5 4 9 4 2 9 7 7 11 8 7 1 16 0 21 5 Wind rose BIVO January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 /media/vedur/BIVO_windrose_2005-2014.pdf