34 results were found for WA 0821 1305 0400 Biaya Borong Pasang Molding Ruang Tamu Kecil Di Tanjung Priok Jakarta Utara.

Results:

• 21. 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

• 22. VI_2014_005

  with vertical boundary-layer profiles calculated di- rectly from HARMONIE model levels. Due to the temporal and spatial variability of model level heights, for the calculation of average vertical profiles, individual model profiles above 6The large positive bias northeast of Vatnajökull is due to the unusually cold summertime temperatures measured at Station 5932, situated near the edge /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 23. Keskitalo_et_al-MLG_and_adaptation_FINAL

  /media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf

• 24. VI_2016_006_rs

  in a collaboration between the Austrian engineering company Ingenieurbüro Illmer Daniel e.U. (DI), Efla consulting engineers and the Icelandic Meteorological Office (IMO). Daniel Illmer carried out the analysis of landslide protection measures, Jón Kristinn Helgason, Tómas Jóhannesson and Eiríkur Gíslason wrote sections about the geographical setting, the land- slide history and the assessment /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 25. VI_2015_007

  with the same method used to estimate qR(D;T ), but instead of pooling AMF series for a given duration D from different sites, the estimation is made individually for each site i by pooling AMF series for different durations D. The index flood, µi(D), is modelled at each site i as a continuous function of D, as follows: 12 µi(D) = µi 1+(D=Di)li ; (6) where µi, Di and li are basin dependent parameters /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

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

  value of the least squares line matched the expected 2010 value based on the AR modelling of the past climate. The trend analysis of the future climate eliminates the di- rect use of a past baseline period in the derivation of the sce- narios and provides a consistent match with the recent cli- mate development. Furthermore, the statistical matching of the past climate observations with the trend /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 27. GA_2009_91A_4_Andreassen

  /media/ces/GA_2009_91A_4_Andreassen.pdf

• 28. Lorenzoni_Pidgeon_2006

  /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 29. Refsgaard_etal-2007-Uncertainty-EMS

  /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 30. VI_2020_004

  /media/vedurstofan-utgafa-2020/VI_2020_004.pdf