30 results were found for WA 0812 2782 5310 Biaya Yang Dikeluarkan Untuk Pemasangan Pintu Kaca Es Cangkringan Sleman.

Results:

• 21. 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

• 22. VI_2021_008

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

• 23. VI_2017_009

  MOHC-HadGEM2-ES GCM v v x MPI-ESM-MR/LR GCM v v v NCC-NorESM GCM x v v RCA4 RCM v v v REMO2009 RCM v v x Table 2. Full names of the GCMs and RCMs listed in Table 1. Model name Full name CCCma-CanESM2 Canadian Centre for Climate Modeling and Analysis. The Second Generation Earth System Model (Chylek et al., 2011). COSMO-CLM4-8-17 Consortium for Small-scale Modeling. Climate Limited /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 24. VI_arsskyrsla2020

  /media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf

• 25. 2010_003rs

  ca ti o n s fo r th e la rg est e a rt h q u a ke s w it h in t h e S IS Z b et w ee n 1 7 0 6 a n d 2 0 0 8 d en o te d b y w h ite fil le d c ir cles. E stim a te d f a u lt p la n es o f h is to ric a l ea rt h q u a ke s a re s h o w n a s w h ite , th ick li n es ( fr o m R o th , 2 0 0 4 ). F a u lt p la n es f ro m 1 9 9 8 ( V o g fj ö rd et a l. , 2 /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 26. Journal_of_Hydrology_Veijalainen_etal

  The hydrological simulations were performed with the Wa- tershed Simulation and Forecasting System (WSFS) developed and operated in the Finnish Environment Institute (Vehviläinen et al., 2005). The WSFS is used in Finland for operational hydrolog- ical forecasting and flood warnings (www.environment.fi/water- forecast/), regulation planning and research purposes (Vehviläinen and Huttunen, 1997 /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 27. 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

• 28. vanRoosmalen_etal-2009-WRR_2007WR006760

  1998] and RCM output such as incoming and outgoing, short- and long-wave radiation, temperature, water vapor pressure, and wind speed: ETref ¼ 0:408D Rn
  Gð Þ þ g 900T þ 273 u2 es
  eað Þ Dþ g 1þ 0:34u2ð Þ ð3Þ where ETref is reference evapotranspiration (mm d
  1), Rn is net radiation at the crop surface (MJ m
  2 d
  1), G is soil heat flux density (MJ m
  2 d
  1), T is mean daily air temperature at 2 m /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 29. VI_2014_006

  /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 30. VI_2020_005

  using Bayesian fingerprinting esti- mates. Dangendorf and Marcos (2018) found a similar linear long term trend since 1902; 1.3 0.2 mm/yr, using a hybrid approach combining various methods. They also estimated the 1993-2012 rate to have been 3.1 1.4 mm/yr which is consistent with previous satellite estimations. Their es- timations show especially large differences from previously reported rates /media/vedurstofan-utgafa-2020/VI_2020_005.pdf