37 results were found for s 건마가자─『텔그DR8899）✻구글광고 건마가자 건마가자도메인 건마가자트위터.

Results:

• 31. Bad weather is expected

  23.2.2017 The Icelandic Meteorological Office wants to emphasize the extremely bad weather that is expected tomorrow Friday 24th of February. Windspeed is expected to be 20 - 28 m/s (45 - 62 miles/hour) in the south and west part after noon, tomorrow with strong gusts up to 40 m/s /about-imo/news/bad-weather-is-expected-1

• 32. Warning - severe storm in the South on Sunday

  Warning - severe storm in the South on Sunday Strong wind gusts 21.2.2015 Forecast Increasing east wind, 10 to 18 m/s in the south, late evening, with snow. Much lighter wind in the north and east, fair and temperatures /about-imo/news/nr/3086

• 33. Weather warning - violent storm

  Weather warning - violent storm 4.12.2015 A strong gale warning (average windspeed above 20 m/s) is in effect in Iceland this afternoon and for most of tomorrow. A violent storm (average wind speed, above 28 m/s) is expected /about-imo/news/nr/3245

• 34. Severe gale or storm

  Severe gale or storm Heaviest rainfall around mountains and ice-caps 19.10.2016 A weather warning was issued yesterday afternoon, Tuesday 18th October, forecasting south and southeast severe gale or storm (average wind speed 20 - 28 m/s) in most of Iceland until /about-imo/news/severe-gale-or-storm

• 35. News

  News © Morten S Riishuus /about-imo/news/bigimg/3453

• 36. ces_SA_group_flyer_new

  series analysis Regional series are compiled based on regions having similar climatological characteristics and streamflow regimes. These series are also useful for evaluating patterns and trends, both in time and by region. Regional series for precipitation, temperature and runoff are being compiled, updated and analysed within the CES project. - 4 0 - 2 0 0 2 0 4 0 6 0 W S P S U M A Q , % - 4 0 /media/ces/ces_SA_group_flyer_new.pdf

• 37. norsem_asdis

  the first tomographic model of Eyjafjallajökull volcano, south Iceland, using ambient noise tomography. The data were collected on a dense network of temporary and SIL seismometers prior to and during the 2010 eruption. Cross-correlations between stations enabled us to construct phase-velocity dispersion curves and create phase-velocity maps, for periods between 1.6-6.5 s /media/norsem/norsem_asdis.pdf