72 results were found for AG包杀网 130—0687—8615 包abwer纱.

Results:

• 31. Update on volcanic activity in Grímsvötn

  except in the northwest. The eruption has abated slightly since yesterday. No effusion of lava has been observed. 22 May 2011 The altitude of the plume is monitored by two weather radars, one located in Keflavík International Airport 220 km from the volcano, and a mobile one currently situated approx. 80 km away from the volcano. Initially the plume reached approx. 20 km altitude but during /earthquakes-and-volcanism/articles/nr/2180

• 32. Bardarbunga_kafli20140825

  an 80 km2 ice-filled caldera. The characteristic activity is explosive basaltic eruptions occurring on central volcano flanks or the fissure swarm. Known eruptions have mostly been VEI 3-4 but occasionally VEI 5-6 (bulk volume of tephra up to 10 km3). The largest eruptions occurred in the early Holocene, effusive basaltic eruptions on the fissure swarm with lava volumes ≥20 km3. Eruption /media/jar/Bardarbunga_kafli20140825.pdf

• 33. ved-eng-2015

  /media/vedurstofan/utgafa/skylduskil/ved-eng-2015.pdf

• 34. The weather in Iceland 2014

  or about 20 percent above the 1961 to 1990 mean. The precipitation was especially heavy in the North and East. At Akureyri 743.7 mm, or 50 percent above the mean. This is the highest annual sum since the beginning of registration in 1928 (although it is only a few mm more than measured in 1989). Table 2. Precipitation overview 2014 station total mm 1961-1990 % 2004-2013 % max 24-hr mm /about-imo/news/nr/3082

• 35. The weather in Iceland 2015

  /about-imo/news/nr/3273

• 36. Markarfljót outwash plain and Öræfajökull

  currents. Because of the wide range of likely flow rheologies, three Manning's n values are assessed: 0.05, 0.1, and 0.15 s/m1/3. Results indicate that a large part of the lowland between the rivers Skaftafellsá and Breiðá (350 km2) is susceptible to flooding because of jökulhlaups descending the western and southern slopes of Öræfajökull. Characterised by average flow velocities in excess of 20 m/s /hydrology/hazard-risk-assessments/glacial-outburst-floods/markarfljotsaurar-oraefajokull/

• 37. Factsheet_Bardarbunga_20150130

  MANAGEMENT  Seismic activity in Bardarbunga continues to be strong. The strongest earthquake since the last meeting of the Advisory Board on last Tuesday was measured M4,6 yesterday, Thursday, at 21:45. Rather strong and flurry wave of seismic activity was recorded in Bardarbunga cauldron yesterday evening between 20:50 and 22:30 Three earthquakes stronger than M4,0 were detected over /media/jar/Factsheet_Bardarbunga_20150130.pdf

• 38. ved-eng-2014

  or about 20 percent above the 1961 to 1990 mean. The precipitation was especially heavy in the North and East. At Akureyri 743.7 mm, or 50 percent above the mean. This is the highest annual sum since the beginning of registration in 1928 (although it is only a few mm more than measured in 1989). Table 2. Precipitation overview 2014 station total mm 1961-1990 % 2004-2013 % max /media/vedurstofan/utgafa/skylduskil/ved-eng-2014.pdf

• 39. Traffc-maintenance_expenditures

  847 2) 59 650 88 048 4) 20 165 9 582 - 8 110 161 728 322 974 636 1 244 770 2002 .. 633 847 2) 54 354 81 892 4) 19 329 9 071 - 4 853 162 705 163 966 014 1 260 860 2001 .. 542 806 2) 81 295 50 734 4) 19 889 9 000 - 5 690 141 203 48 850 666 1 132 021 2000 .. 533 629 2) 125 273 32 157 4) 23 190 6 997 - 5 332 115 674 197 842 483 1 149 476 1999 .. 526 558 2) 141 789 8 744 4) 26 555 6 463 14 403 2 827 109 /media/loftslag/Traffc-maintenance_expenditures.pdf

• 40. Hare-2011-ParticipatoryModelling

  stage )Suppor t an d ski lls n ee de d Har e et a l. (2003 ) X X An aly se lin ks be tw ee n participator y structur e an d proces s implementatio n Ba rr et ea u et a l. (2010 ) X X X Pr o vid e cle ar de sc rip tio n o fproces s (m an ag e ex pe ct at io n s); monitorin g an d evaluatio n Bot s an d va n Daale n (2008 ) X X X X X Su pp o rt pr o ce ss de sig n Ad ap te d fra m ew o rk u se d in th /media/loftslag/Hare-2011-ParticipatoryModelling.pdf