51 results were found for WA 0821 1305 0400 Biaya Yang Diperlukan Untuk Membangun Rumah 5 X 10 Murah Johar Baru Jakarta Pusat.

Results:

• 21. Alam_Ashraful_CES_2010

  Short distance transportation Long distance r g y i n p u t o x i d e E m i s M W h - 1 8 4 - M5 (-20%) M6 (-30%) Energy wood in power plant Timber in pulp and saw mill transportation Chipping s i o n s K g C O 2 (b) Norway spruce: Myrtillus type 10 l a r e a ( m 2 h a - 1 ) Basal area just before thinning Remaining basal Thinning threshold Energy wood thinning 8 9 B a s a l /media/ces/Alam_Ashraful_CES_2010.pdf

• 22. 2005EO260001

  lake within the caldera until the surrounding ice is breached. When that happens, water escapes to cause a jökulhlaup in the river Skeidará, after having traveled ~50 km beneath the Skeidarárjökull outlet glacier (Figure 1b). Jökulhlaups occur there every 1–10 years and last from days to weeks, each time releasing 0.4–4 km3 of water [Björnsson, 2002]. Volcanic eruptions in Gríms- vötn often /media/jar/myndsafn/2005EO260001.pdf

• 23. Gradual fading of seismic activity at Bárðarbunga and the dyke intrusion

  decreased by a factor of 5 to 10 (maximum) and some of the data is still under revision due to the high numbers of earthquakes. While the number of magnitude 5 earthquakes (red dots) has obviously decreased, there is still a significant number of earthquakes between M3 and M5 detected to this day. A first interpretation might be, that rock parameters like the friction on the ring fault could have /earthquakes-and-volcanism/articles/nr/3039

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

  ). 24. M. E. Moss, Water Resour. Res. 15, 1797 (1979). 25. E. Ehrlich, B. Landy, Public Works, Public Wealth (Center for Strategic and International Studies Press, Washington, DC, 2005). 26. United Nations General Assembly, U.N. Millennium Declaration, Resolution 55/2 (2000). 10.1126/science.1151915 –40 –20 –10 –5 –2 40201052 Human influences. Dramatic changes in runoff volume from ice-free land /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 25. Journal_of_Hydrology_Veijalainen_etal

  at 67 sites: (a) 100-year floods with the Gumbel distribution and (b) average discharge. −6 0 −4 0 −2 0 0 20 40 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 Scenario number Change in 100a Flood (% ) Fig. 5. Box plot (median, 25 and 75 percentiles, average [diamond], max and min) of changes in 100-year floods in 2070–2099 at the 67 sites with different scenarios. Numbering of the scenarios /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 26. 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

• 27. 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

• 28. 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

• 29. 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

• 30. 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