85 results were found for WA 0821 7001 0763 (FORTRESS) Pintu Baja Ukuran 120 Tanjung Bringin Kabupaten Semarang.

Results:

• 61. ice-chart_colour-code-standard

  -250-130 FY thin ice (white ice) first stage 2.5.1.1 175-250-000 FY thin ice (white ice) second stage 2.5.1.2 000-200-020 FY medium ice 2.5.2 000-120-000 FY thick ice 2.5.3 180-100-050 Old ice 2.6 255-120-010 Second-year ice 2.6.1 200-000-000 Multi-year ice 2.6.2 150-150-150 Fast ice of unspecified SoD 2.6 210-210-210 Ice shelf 10.3 255-255-255 Ice of undefined SoD - 255-255-255 Drifting ice of land /media/hafis/frodleikur/ice-chart_colour-code-standard.pdf

• 62. 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

• 63. AnneFleig_May2010_CES

  drought-supporting WTs over previous n days (n = 1, 15, 30, 45, 60, 90, 120, ... 330). Determination of the period of influence: dreg 90 45 little groundwater45 45 CES conference, Oslo, Norway, 31 May - 2 June 2010 210 60 45 60 highly productive aquifers moderately productive aquifers}90 210 60 60 Anne K. Fleig et al. “Regional hydrological droughts and weather types in north-western Europe /media/ces/AnneFleig_May2010_CES.pdf

• 64. Bárðarbunga 2014 - November events

  graph has a sixfold exaggeration of the vertical axis and on the upper one the difference in hight is multiplied by a factor of 120. The intention is not to make an image which resembles the volcano but to distinguish clearly and graphically between the results derived after each surveillance flight. Eight flight measurements are shown, from 5 September to 26 November 2014. The Institute of Earth /earthquakes-and-volcanism/articles/nr/3023

• 65. Bardarbunga-2014_November-events

  repeatedly. For convenience, the results are presented schematically, see below. The lower graph has a sixfold exaggeration of the vertical axis and on the upper one the difference in hight is multiplied by a factor of 120. The intention is not to make an image which resembles the volcano but to distinguish clearly and graphically between the results derived after each surveillance flight. Eight /media/jar/Bardarbunga-2014_November-events.pdf

• 66. Bárðarbunga 2014 - November events

  graph has a sixfold exaggeration of the vertical axis and on the upper one the difference in hight is multiplied by a factor of 120. The intention is not to make an image which resembles the volcano but to distinguish clearly and graphically between the results derived after each surveillance flight. Eight flight measurements are shown, from 5 September to 26 November 2014. The Institute of Earth /earthquakes-and-volcanism/articles/nr/3023/

• 67. VI_2022_006_extreme

  /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 68. VI_2020_008

  /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 69. VI_2016_006_rs

  /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 70. VI_2014_001

  –31Aug), and years with more than 120 days of missing data were omitted. For instantaneous flow series, AMF series were extracted from the monthly maxima and years with more than four missing months omitted. 2.3 Meteorological data Gridded daily precipitation (Crochet et al., 2007), 2m air temperature (Crochet and Jóhannesson, 2011), 10m wind-speed, vapor pressure and incoming short wave radiation /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf