68 results were found for 海洋之神充20送20【┃咨询Ｑ２17⒋31】】.

Results:

• 11. Web-pages on the Eyjafjallajökull eruption 2010

  January 2011 Eyjafjallajökull eruption 2010 - the role of IMO - 21 December 2010 Update on activity in Eyjafjallajökull assessment from 14 April until 9 October 2010 QA on the eruption in Eyjafjallajökull, Iceland - 17 April Forecast for volcanic ash fall in Iceland - updated from 20 April until 23 May Photos from Eyjafjallajökull - 9 May An eruption in South Iceland - 23 March Photo galleries /earthquakes-and-volcanism/articles/nr/2221

• 12. BIGR_windrose_2005-2014

  ) 0 5 10 15 20 25 0 45 90 135 180 225 270 315 360 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 52 49 35 28 30 23 20 42 5 2 34 61 48 31 35 17 15 19 15 9 7 10 9 11 22 43 2 1 8 10 20 4 5 16 6 9 17 3 3 Wind rose BIGR December 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 /media/vedur/BIGR_windrose_2005-2014.pdf

• 13. BIKF_windrose_2005-2014

  89 7 72 0 47 7 29 7 32 3 43 8 40 2 40 2 40 5 44 3 52 3 79 1 67 4 51 3 43 9 34 6 31 1 28 3 29 9 40 5 45 3 45 8 39 1 25 2 29 0 20 1 18 0 19 6 22 4 19 2 19 6 21 8 17 3 29 4 Wind rose BIKF May 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 7 Frequency of wind direction (%) Aerodrome Total /media/vedur/BIKF_windrose_2005-2014.pdf

• 14. Grímsvötn 2010

  increased by 1 metre during 20 hours (from 14 PM Oct. 31 to 10 AM Nov. 1). Since the floodwaters dig into the river bed, spread out and frequently change their course it must be kept in mind that the water level measured at a fixed location can only be viewed as an indicator of discharge. More extensive and repeated measurements at several places are therefore needed during jökulhlaups to determine /hydrology/articles/nr/2040

• 15. Grímsvötn 2010

  increased by 1 metre during 20 hours (from 14 PM Oct. 31 to 10 AM Nov. 1). Since the floodwaters dig into the river bed, spread out and frequently change their course it must be kept in mind that the water level measured at a fixed location can only be viewed as an indicator of discharge. More extensive and repeated measurements at several places are therefore needed during jökulhlaups to determine /earthquakes-and-volcanism/articles/nr/2040

• 16. Bárðarbunga 2015 - February events

  the last report yesterday morning, the strongest was M3.7 yesterday afternoon at 15:20. All in all about 25 earthquakes were detected. About 20 events occurred in the dyke intrusion, all of them smaller than M1.2. Four events were measured around Askja and three around Herðubreið. 21 February 2015 - aerial photos from the first five months Well shaped The crater 31 January 2015 /earthquakes-and-volcanism/articles/nr/3087

• 17. Bárðarbunga 2015 - February events

  the last report yesterday morning, the strongest was M3.7 yesterday afternoon at 15:20. All in all about 25 earthquakes were detected. About 20 events occurred in the dyke intrusion, all of them smaller than M1.2. Four events were measured around Askja and three around Herðubreið. 21 February 2015 - aerial photos from the first five months Well shaped The crater 31 January 2015 /earthquakes-and-volcanism/articles/nr/3087/

• 18. Bardarbunga-2015_February_events

  the monthly articles give an overview of events: August, September, October, November December, January, February, March and the overview article (list of links). Calendar Below is a calendar with a short-cut to each day of the month. Feb: 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 Panoramic view towards the eruptive site in Holuhraun 3rd September 2014. Photo /media/jar/Bardarbunga-2015_February_events.pdf

• 19. Johannesson_Thomas_CES_2010

  Nigardsbrevatn annual discharge 0 5 10 15 1951 1971 1991 2011 2031 2051 2071 2091 m 3 / s year DMI ECHAM A1b with gls DMI ECHAM A1b without gls met.no HADLEY A1b with gls met.no HADLEY A1b without gls SMHI BCM A1b with gls SMHI BCM A1b without gls Discharge seasonality, HBV/GLS models 25 30 35 40 Nigardsbrevatn daily mean discharge 0 5 10 15 20 1. jan. 20. feb. 11. apr. 31. mai. 20. jul. 8. sep. 28. okt. 17 /media/ces/Johannesson_Thomas_CES_2010.pdf

• 20. VI_2014_001

  ............................................... 24 4.2.2 Index flood modeling and prediction ................................................ 26 4.2.3 Flood quantiles prediction ............................................................. 27 5 Conclusion and future research ...................................................................... 31 6 Acknowledgements /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf