78 results were found for 平心在线假线私网 191-1999-2299 圣noiw安eF.

Results:

• 11. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  ¨kull ice caps and at nunataks. Airborne radar altimetry surveys have been conducted in the accumula- tion areas of the nearby My´rdalsjo¨kull in May and September
  November each year since October 1999 and Fig. 2 Shaded relief images of the Eyjafjallajo¨kull (E), Tindfjallajo¨kull (Ti), Torfajo¨kull (To) and My´rdalsjo¨kull ice caps and surrounding glacier free areas, based on digital elevation maps /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 12. Reports and publications

  (PDF) Bergþóra S. Þorbjarnardóttir, Gunnar B. Guðmundsson, Steinunn S. Jakobsdóttir 6 1,8 2003 Continuous GPS neasurements in Iceland 1999 - 2002 (PDF) Halldór Geirsson 94 3,9 2003 The South Iceland earthquakes 2000 - a challenge for earthquake prediction research (PDF) Ragnar Stefánsson, Gunnar B. Guðmundsson, Páll Halldórsson 21 0,5 2003 PREPARED - Management and resource /earthquakes-and-volcanism/reports-and-publications/

• 13. Water_resources_man_Veijalainen_etal

  hydrological changes due to climate change, since relatively modest increases in temperature can result in substantial changes in runoff patterns (Arnell 1999; Lettenmaier et al. 1999; Payne et al. 2004). Previous studies on climate change impacts (Beldring et al. 2006; Silander et al. 2006; Vehviläinen and Huttunen 1997) have found that during warmer winters with more rain and increased snowmelt winter /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 14. Sigurður Th. Rögnvaldsson

  died in a car accident in October 1999. Sigurður graduated from the Menntaskólinn við Hamrahlíð junior college in 1982 and received his BS degree in geophysics from the University of Iceland in 1987. During his undergraduate years, Sigurður worked summers at the Icelandic Energy Authority, carrying out electromagnetic resistivity survey and other field work for geothermal prospecting. Sigurður /earthquakes-and-volcanism/conferences/jsr-2009/sigurdur/

• 15. Sigurður Th. Rögnvaldsson

  died in a car accident in October 1999. Sigurður graduated from the Menntaskólinn við Hamrahlíð junior college in 1982 and received his BS degree in geophysics from the University of Iceland in 1987. During his undergraduate years, Sigurður worked summers at the Icelandic Energy Authority, carrying out electromagnetic resistivity survey and other field work for geothermal prospecting. Sigurður /earthquakes-and-volcanism/conferences/jsr-2009/sigurdur

• 16. The ice cap Snæfellsjökull is thinning rapidly

  in recent years according to people living in the neighbourhood of the glacier and travellers in the area, which is among the most popular tourists' destinations in Iceland. By comparing airborne lidar measurements of the glacier surface, that were carried out in September 2008, with a digital terrain model by the mapping company Loftmyndir ehf from 1999, the average lowering of the ice surface /weather/articles/nr/1618

• 17. The ice cap Snæfellsjökull is thinning rapidly

  in recent years according to people living in the neighbourhood of the glacier and travellers in the area, which is among the most popular tourists' destinations in Iceland. By comparing airborne lidar measurements of the glacier surface, that were carried out in September 2008, with a digital terrain model by the mapping company Loftmyndir ehf from 1999, the average lowering of the ice surface /weather/articles/nr/1618/

• 18. Earthquakes and pre-earthquake processes

  pre-earthquake processes and earthquake prediction research. The conference will be held on October 30th 2009 in Reykjavík, Iceland, and is dedicated to the memory of Sigurður Th. Rögnvaldsson, geophysicist, who died on 25th October 1999. He was highly respected in earthquake research in Iceland /about-imo/news/nr/1695

• 19. VI_2009_013

  mechanisms and the relationship between b-values and source depth is examined. During the analysis period, three major swarms were recorded. Two of the swarms, in 1994 and 1999–2000, occurred in the upper crust and were accompanied by crustal deformation. No uplift was detected during the third swarm, which occurred in 1996 near the crust mantle boundary, between 19 and 25 km depth /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 20. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  need inclusion (van der Keur et al. 2008). The complete suite of uncertainties has been referred to as the uncertainty cascade (Hulme and Carter 1999; Katz 2002; Foley 2010). Making climate change adaptation decisions is particularly difficult since they rely on uncertainties related to climate projections as well as to developments in natural systems and sectors that are affected by other /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf