72 results were found for 菲律宾圣安娜假盘菲律宾圣安娜假线【191-1999-2299】圣noiw安Fc2kG.

Results:

• 11. 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/

• 12. 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

• 13. 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

• 14. Earthquake activity in Katla volcano October 2011

  The current period of unrest began in July 2011, when a short-lived glacial flood burst from Mýrdalsjökull in connection with increased seismicity. Since then, several hundred micro-earthquakes have taken place within the area of the caldera. The enclosed graph shows how the ongoing activity compares to earlier episodes of seismic unrest at Katla in 1999 and 2002-2004. In the early hours /about-imo/news/nr/2360

• 15. VI_2015_009

  series were extracted for each hydrological year (taken here from Sept 1 to Aug 31), from monthly max- imum instantaneous flow series. Years with more than two missing months were omitted. As the AMF of year 1999 at gauging stations vhm102 and vhm233 was strongly suspected to be caused by a jökullhlaup, the 2nd largest annual flow was selected for this year. One must bear in mind that uncertainties /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 16. Eriksson_1-Risk-perception

  environmentalism (e.g., purchase, use and disposal), others (e.g., organizational behaviours) • An indirect effect of risk perception (or problem awareness) on pro-environmental behaviour (e.g., the value belief norm theory (Stern et al., 1999), the theory of planned behaviour (Ajzen, 1991)) 8 (2) Value-belief-norm theory of environmentalism (VBN) Values Beliefs Personal norm Behaviour /media/loftslag/Eriksson_1-Risk-perception.pdf

• 17. VI_2009_006_tt

  known in other locations 3 (Björnsson, 1976). Generally, jökulhlaups from marginal lakes have decreased due to thinning of glaciers during the twentieth century because lower ice dams cause the lakes to burst at a lower water level. This leads to smaller but more frequent jökul- hlaups. Other types of floods can also originate in marginal glacier lakes. For example, a flood in the river Farið in 1999 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 18. Protective measures

  to avalances: An overview of the need for avalanche protection measures in Iceland (IMO Rep. 96004, 1996, authors T. Jóhannesson, K. Lied, S. Margreth and F. Sandersen) [summary of IMO publication 96003/96004] (html) Adaptation of the Swiss Guidelines for supporting structures for Icelandic conditions (IMO Int. Rep. 99013, 1999, authors T. Jóhannesson and S. Margreth) (pdf 0.1 Mb) Addendum /avalanches/imo/protective/

• 19. vonKorff_etal-2010

  a prerequisite and an element of good governance and the sustainable management of natural resources” (Enserink et al. 2007, similar to Pahl-Wostl et al. 2008). The issue of public participation is becoming more important not only in natural resources management (Syme and Sadler 1994, Chess and Purcell 1999, Webler and Tuler 1999, Beierle and Konisky 2000, Bryner 2001, Webler and Tuler 2001, Beierle /media/loftslag/vonKorff_etal-2010.pdf

• 20. The weather in Iceland in 2018

  Grímsstaðir 473,7 134,9 113,2 20,0 197 110 Dalatangi 1975,2 131,7 112,1 71,3 275 189 Höfn í Hornafirði 1874,7 139,7 121,7 56,4 281 191 Vatnsskarðshólar 2016,4 123,9 116,5 57,1 266 210 Hjarðarland 1319,2 98,4 103,5 52,7 204 174 Írafoss 2191,0 120,8 /about-imo/news/the-weather-in-iceland-in-2018