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51 results were found for WA 0821 1305 0400 RAB Konblok Taman Cluster Perumahan Terpercaya Penjaringan Jakarta Utara.


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  • 31. VI_2013_006

    the lightning cluster 10‒20 km to the north. The same wind correction as applied for 2011 moves the eruption site estimate to about 4 km WNW of the correct site. By applying a smaller wind correction (time constant of 200 s instead of 500 s) gives a perfect match for Eyjafjallajökull for the day with the highest frequency of volcanic lightning (16 May 2010). 13 Figure 7 /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf
  • 32. AnneFleig_May2010_CES

    British and 22 Danish stations; • natural or naturalized daily streamflow data for 1964–2001; • threshold level method barb2right at-site drought. • cluster analysis barb2right six regions. Anne K. Fleig et al. “Regional hydrological droughts and weather types in north-western Europe “ University of Oslo Droughts WTs SummaryRelationsIntroduction Outlook Regional hydrological drought Regional /media/ces/AnneFleig_May2010_CES.pdf
  • 33. 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
  • 34. VI_2021_008

  • 35. 2010_003rs

  • 36. 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
  • 37. 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 ied .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
  • 38. 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
  • 39. Bárðarbunga 2015 - February events

    : Around a dozen earthquakes have been detected around the caldera rim, the strongest one was M3.9 yesterday at 14:12. Dyke intrusion: Six earthquakes were observed in the dyke intrusion, all of them M<1.5. Other regions: A M2.2 earthquake occurred east of Herðubreið today at 03:29, all together around 10 events were detected in the same cluster. 15 February 2015 12:00 - from geoscientist /earthquakes-and-volcanism/articles/nr/3087
  • 40. Bárðarbunga 2015 - February events

    : Around a dozen earthquakes have been detected around the caldera rim, the strongest one was M3.9 yesterday at 14:12. Dyke intrusion: Six earthquakes were observed in the dyke intrusion, all of them M<1.5. Other regions: A M2.2 earthquake occurred east of Herðubreið today at 03:29, all together around 10 events were detected in the same cluster. 15 February 2015 12:00 - from geoscientist /earthquakes-and-volcanism/articles/nr/3087/

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