79 results were found for WA 0821 1305 0400 RAB Pembangunan Rumah Type 36/60 1 Lantai Jakarta Pusat.

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. 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

  08:21 03:49, n/a 09:20 UTC 59–340 minutes Hekla Feb. 26, 2000 hau 17:13 17:21 18:08 18:08 18:16 18:20 18:19 UTC 11 minutes Grímsvötn Nov. 1, 2004 skr 19:08 19:09 19:48 19:35 19:35 19:53 ~20:00 UTC ~25 minutes Eyjafjallajökull April 14, 2010 mid 02:38, 08:03 02:36, 08:00 02:32, 07:59 n/a, 08:14 03:05, 08:14 n/a, 08:55 ~06:50 UTC ~258 minutes Grímsvotn May /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. 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

• 6. Isskyrsla_20101212

  örugt að fara fyrir Horn í um 10 sml frá landi en það yrði að hafa góðan útvörð. Kl.1341, kalla TFB og spyr um ETA í RVK, ETA um kl 1440. Kl 1305, AIS umferð fyrir N- Horn. Vegna bilunnar í WS 1 var megináhersla lögð á ískönnun í þessu flugi. Flugskýrsla TF-SIF 12. desember 2010 Flug nr. 117410.025 Ískönnun. Meginröndin lá um eftirtalda staði. 1. 67°47.0N 023 /media/hafis/skyrslur_lhg/Isskyrsla_20101212.pdf

• 7. 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

• 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. 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

• 10. Kok_JGEC658_2009

  scenario development, with an example from Brazil Kasper Kok * Land Dynamics, Department of Environmental Sciences, Wageningen University, P.O. Box 47, 6700 AA Wageningen, The Netherlands 1. Introduction The world is undergoing rapid changes while globalising constantly, which gives the consideration of the future new urgency and importance. Scenario development has emerged as a key method when taking /media/loftslag/Kok_JGEC658_2009.pdf