19 results were found for WA 0821 1305 0400 Berapa Biaya Pasang Kanopi Teras Cor Terpercaya Kembangan Jakarta Barat.

Results:

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

  1936, 1946, 1989, 2001, 2008 and 2010, mass balance observa- tions conducted in 1936–1938 and after 2001, energy bal- ance measurements after 2001, and glacier surface velocity derived by kinematic and differential GPS surveys and cor- relation of SPOT5 images. The approximately 20 % volume loss of this glacier in the period 1895–2010 is realistically simulated with the model. After calibration /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 12. Kok_JGEC658_2009

  /media/loftslag/Kok_JGEC658_2009.pdf

• 13. ces-glacier-scaling-memo2009-01

  for the glaciers in question can be made, based on mass balance and ice thickness estimates for the glaciers in the group, Equation (13) can be used to make cor- rections to k. If the response time according to Equation (13) is too low, Equation (4) indicates that be is too negative and the glaciated area has thus been reduced too much at the lowest alti- tudes. Then the value of k needs /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 14. 2010_017

  m J M5 [C°] -3 obs. [C°] -4 nce 1 re 5. Comp 26); an int temperatu this system y gridded v picion abo -Jökulsá w similar dif han observ h elevation ces the effe months No ly only on high the tem n band wi refore be s onthly tem an Feb Ma .2 -3.1 -3. .3 -4.1 -3. .1 1.0 0.6 arison of m erpolation re is shown atic differe alues, see T ut the qual atershed; b ference wa ations for t gradient fo /media/ces/2010_017.pdf

• 15. VI_2021_008

  /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 16. Refsgaard_etal-2007-Uncertainty-EMS

  probability distribu- tions and correlations are usually poorly known. Ignoring cor- relations and co-variance in input distributions may lead to substantial under- or over-estimation of uncertainty in model outcome. Advanced sampling methods have been designed such as Latin Hypercube sampling to reduce the required num- ber of model runs needed to get sufficient information about the distribution /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 17. Hare-2011-ParticipatoryModelling

  ea th , th e m et ho d u se d at th is st ag e fo r th es e st ak eh o ld er typ es is sp ec i
  ed .Sh oul d ther e be tw o o r mor e model sbein g develope d in th e process ,the n th e typ e o fmode lt o whic h th e metho d wa s applie d is show n in parentheses .O T re fe rs to th e co m po si tio n o ft he o rg an iz in g te am . Fo r o rg an iz in g te am in vo lve m en t in di ffe re n t pa rt /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 18. 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

• 19. 2013_001_Nawri_et_al

  mAGL, based on the original and cor- rected WRF model data, is shown in Figure 6. Along the coast, with a good coverage of station data, differences between corrected and original values are of the same magnitude as the local differences between the measured and original model values at 10 mAGL. In winter, wind power density over the highest points of near-coastal terrain in the western part /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf