16 results were found for WA 0821 1305 0400 RAB Paving Anti Lumut Segi 6 Bogor Barat Kota Bogor.

Results:

• 11. VI_2021_008

  a coherent, emergent signal in RSAM data (see Figure 2), raising the question: Can RSAM data be empirically used to detect volcanic tremor events preceding eruptions? 6 Figure 1. Photo of the monitoring setup in the IMO’s natural hazards monitoring room. The right screen shows real-time earthquake and tremor data. Tremv output is displayed in red box with the last 24 hrs of all frequency /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 12. Hare-2011-ParticipatoryModelling

  Dispatch: 02.08.11 CE: E E T 5 9 0 No. of Pages: 19 ME: 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 Another possible driving force behind its popularity is changing legislation requiring environmental managers and policy-makers to increase stakeholder participation in their work [e.g /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 13. Observations - Kollaleira í Reyðarfirði

  Observations - Kollaleira í Reyðarfirði | Observations | Icelandic Meteorological office Observations - Kollaleira í Reyðarfirði Mon 1.05 13 GMT 4.8° WNW 4 Max wind : 4 / 7 12 GMT 4.4° NW 3 Max wind : 3 / 6 11 GMT 3.5° NW 4 Max wind : 4 / 7 10 GMT 3.7° W 3 Max wind : 3 / 6 09 GMT 2.6° WSW /m/observations/areas

• 14. Forecasts - Skarðsfjöruviti

  Forecasts - Skarðsfjöruviti | Station forecasts | Icelandic Meteorological office Forecasts - Skarðsfjöruviti Mon 1.05 14 GMT 8° E 5 Cloud cover: 100% 15 GMT 8° E 6 Cloud cover: 100% 16 GMT 7° E 5 Cloud cover: 100% 17 GMT 7° E 6 Cloud cover: 100% 18 GMT 7° E 6 Cloud cover: 100% 19 /m/forecasts/areas

• 15. VI_2009_006_tt

  Íslands Bústaðavegur 9 150 Reykjavík   Abstract Fast-rising jökulhlaups from the geothermal subglacial lakes below the Skaftá caul- drons in Vatnajökull emerge in the Skaftá river approximately every year with 45 jökulhlaups recorded since 1955. The accumulated volume of flood water was used to estimate the average rate of water accumulation in the subglacial lakes during the last decade as 6 Gl /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 16. BIHN_windrose_2005-2014

  Wind rose BIHN 2005 − 2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 1 2 3 4 5 6 Frequency of wind direction (%) Aerodrome Total observations: 28301 Calm: 5.3% Variable winds: 1.6% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 2 4 6 8 10 0 45 90 135 180 225 270 315 360 N E S /media/vedur/BIHN_windrose_2005-2014.pdf