78 results were found for WA 0821 1305 0400 Tempat Pasang Pintu Spandrel Aluminium Ukuran Standard Cibarusah Kab Bekasi.

Results:

• 61. Adalgeirsdottir-etal-tc-5-961-2011

  of the sections and the terminus position at the different times. Fig. 5. Winter, summer and annual balance measured at Hoffellsjökull and Breiðamerkurjökull. Measurements from the 1930s expedition (at the lowest stakes only annual balance was measured and therefore winter balance set to zero) are shown with black symbols. The red dots show the average and standard deviation of the mass balance /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 62. GA_2009_91A_4_Andreassen

  data from Fokstua/Fokstugu using monthly lapse rates (as shown in Fig. 3a–b). A lin- ear temperature lapse rate of 0.65°C/100 m was applied at all glacier altitudes. A constant value oftransmissivity, τ, of 0.43 was chosen based on measurements of the AWS in the main ablation season. Daily values of QTOA wer calculated us-ing standard formula. The constants c0 and c1 werederived from eq. 3 using /media/ces/GA_2009_91A_4_Andreassen.pdf

• 63. IMO_AnnualReport2014

  lava field (1 September 2014). In addition to standard weather param- eters (such as precipitation, temperature, and wind), Harmonie also simulates snow accumulation, runo?, evaporation, and more. I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4 9 The weather in Iceland 2014 The year 2014 was warm for most of the year, precipitation was abundant and the sunshine /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 64. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

  ). In the last thirty years, however, this behavioral hypothesis has received considerable challenge from both field researchers and experimentalists. A hugely influential article by Garrett Hardin (1968) highlighted two standard responses to the “tragedy of the commons”: when open-access resources are overexploited, the “an- swer” was to either privatize the resource (in order to realize /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf

• 65. Refsgaard_2-uncertainty

  - nitrate reduction in underground medium medium large large large Model technical uncertainty - numerical approximation small small medium small - bugs in software medium medium small SUM: Importance Type of uncertainty Error propagation Box 1 Error propagation rules using standard deviation (σ ) Addition and Subtraction: z = x + y + .. or z = x - y - .. ..)()( 22 ++= yxz σσσ /media/loftslag/Refsgaard_2-uncertainty.pdf

• 66. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  infrastructur e Me d Hydrology+contex t Epistemic + Aleator y Changin g buildin g desig n standards ,highe rus e o n til e pipe s(structural ) Me d P C M L Sam e as fo rimpac t Increasin g ris k o fhea twave s W ate r suppl y standard s ar e no tme t Me d Contex t(desig n an d operatio n practices ) Aleatory + Ambiguit y Us e o fintermediat e coolin g system s o n wate r suppl y (non-structural ) Lo w /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 67. Lorenzoni_Pidgeon_2006

  ”); standard deviations are in brackets. Psychometric characteristics Climate change Unknown consequences 4.13 (0.88) Risks to future generations 4.31 (0.73) Dread 3.06 (1.12) Well informed 2.80 (1.14) Control any risks to myself 2.48 (1.07) Unfair distribution of risks 3.00 (1.00) Moral concerns 3.44 (1.03) (Source: Poortinga and Pidgeon, 2003a). change (i.e. the ‘dread’ factor in the classic /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 68. VI_2020_011_en

  /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 69. VI_2015_006

  Meteorological Office (IMO) between 2011 and 2014. The model do- main is also the same as for the IMO operational runs, with 300 240 horizontal grid points cov- ering the whole of Iceland and parts of the surrounding ocean, and with a horizontal grid-point spacing of about 2.5 km in both directions. The model is run with the standard 65 vertical levels, and with a non-hydrostatic dynamic core /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 70. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf