47 results were found for WA 0812 2782 5310RAB Vinyl Flooring Rumah Minimalis 5 X 10 Wilayah Jebres Solo.

Results:

• 21. raisanen_ruosteenoja_CES_D2.2

  ............................................................................................................ 4 3. Best estimates of temperature and precipitation change................................................ 7 4. How certainly will temperature and precipitation increase? ....................................... 10 5. Uncertainty ranges and quantiles of temperature and precipitation change .............. 12 6. Hindcast verification of the resampling ensemble /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf

• 22. Lawrence_Deborah_CES_2010

  ECHAM4/OPYC3 NorClim/HIRHAM 25x25 km 'Empirical Adjustment' to 1 x 1 km 100 150 200 250 300 350 400 450 500 550 600 650 700 750 800 850 900 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 ) 1981-2010 GEV from annual max series 2021-2050 GEV from annual max series 2021 - 2050 Annual maximum series 1981 - 2010 Annual maximum series 1981-2010 200-year flood 2021 /media/ces/Lawrence_Deborah_CES_2010.pdf

• 23. Kok_1-scenarios-lecture-1

  .. But with caution Spatial scale Modifiable Areal Unit Problem (MAUP) Ecological fallacy: The mistake of assuming that where relationships are found among aggregate data, these relationships will also be found among individuals or households, or vice versa. Key concepts (from ecology) Forest cover Population density y = -20.1Ln(x) + 60 R2 = 0.84 0 20 40 60 80 100 0 5 10 15 Population density F o re /media/loftslag/Kok_1-scenarios-lecture-1.pdf

• 24. VI_2014_001

  and predicted flood quantiles were compared at gauged sites only, treated as un- gauged, for average recurrence intervals T of 2, 5, 10, 20, 50 and 100 years. The performance of the prediction was evaluated by cross-validation at independent sites not used in the method de- velopment, by calculating the mean relative error (BIAST ) and relative root mean squared error (RMSET ): BIAST (%) = 1 N N /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 25. VI2010-006_web

  fjölbýlishús, skóla, sjúkrahús) og íbúðarhús með fleiri en fjórum íbúðum. 1Ef staðaráhætta er minni en 5 ·10−4 á ári. á því að einstaklingur sé í húsi þegar ofanflóð fellur og til þess hve sterkt húsið er fæst mat á raunáhættu. Ekki er tekið tillit til rýminga eða annarra tímabundinna varúðarráðstafana við gerð hættumats. Yfirvöld hafa ákveðið að áhættan 0.2 · 10−4 á ári eða minni sé viðunandi (ásættan- leg /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf

• 26. ces-glacier-scaling-memo2009-01

  and ice caps may be derived from data about the area distribution of ice bodies in the drainage basin. Since the exponents g in the volume–area scalings v = csg for both ice caps and glaciers TóJ 3 5.12.2009 Memo Area (km2) Volume (km 3 ) 50 100 50 100 150 200 250 50 100 150 200 250 a71 a71a71 a71 a71 10 50 500 500020 1000 1 5 10 0 100 0 2 2 0 20 0 200 0 100 10000 Icelandic ice /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 27. 2013_001_Nawri_et_al

  . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 67 A.14 Þorlákshöfn . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 69 5 List of Figures 1 Topographic map of Iceland with the locations of test sites . . . . . . . . . . . . . 10 2 Annual modelled wind speed distributions and Weibull fits . . . . . . . . . . . . . 16 3 Annotated example of a wind atlas (.lib) text file /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 28. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

  advantageous inequity aversion is relevant for the second mover’s utility, which can be written as: ui2 = 10 − xi2 + 0.8 (x1 + xi2)− βi (x1 − xi2) (3) The second mover should contribute the same amount as the first mover to the public good if her degree of advantageous inequity aversion is such that βi ≥ 0.2. The equilibrium decision of the second mover is written as: x∗i2 =  0 if βi < 0.2 x1 if βi /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 29. Observations - Húsafell

  Observations - Húsafell | Observations | Icelandic Meteorological office Observations - Húsafell Mon 1.05 14 GMT 7.9° NE 5 Max wind : 5 / 8 13 GMT 6.0° NNE 4 Max wind : 6 / 9 12 GMT 4.2° NNE 5 Max wind : 6 / 10 11 GMT 3.2° NNE 5 Max wind : 6 / 11 10 GMT 2.5° NNE 5 Max wind : 6 / 10 /m/observations/areas

• 30. CES_D2.4_task1

  2010) is estimated. x Finally, Gaussian kernel smoothing (Equation (10) in Räisänen and Ruokolainen 2008a) is applied to convert the discrete frequency distribution of the extrapolated observations to a continuous probability distribution. The data sets used, the derivation of the regression coefficients and the Gaussian kernel smoothing are discussed in Appendices A.1-A.3 /media/ces/CES_D2.4_task1.pdf