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• 41. Glossary

  We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below: A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö A A: Icelandic abbreviation of East (compass direction, easterly, eastern). ANA: Icelandic abbreviation of Eastnorthesast (compass direction). ASA: Icelandic /weather/articles/nr/1208

• 42. Glossary

  We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below: A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö A A: Icelandic abbreviation of East (compass direction, easterly, eastern). ANA: Icelandic abbreviation of Eastnorthesast (compass direction). ASA: Icelandic /weather/articles/nr/1208/

• 43. A large landslide falls in Hítardalur valley

  displacements and might be an old landslide deposit. The displaced material is a mixture of e.g. rock debris, scree from the lower part of the hillside, swamp soil and sediments from ancient lakes on the valley bottom. A preliminary estimate of the volume of the slide is 10–20 million m3. The area of the debris tongue is ca. 1,5 km2 and the debris is up to 20–30 m thick. The thickness is 5–10 m in many /about-imo/news/a-large-landslide-falls-in-hitardalur-valley

• 44. A large landslide falls in Hítardalur valley

  displacements and might be an old landslide deposit. The displaced material is a mixture of e.g. rock debris, scree from the lower part of the hillside, swamp soil and sediments from ancient lakes on the valley bottom. A preliminary estimate of the volume of the slide is 10–20 million m3. The area of the debris tongue is ca. 1,5 km2 and the debris is up to 20–30 m thick. The thickness is 5–10 m in many /about-imo/news/a-large-landslide-falls-in-hitardalur-valley/

• 45. VI_2009_012

  to use the available new estimates Mw(v) to build a PGA relationship that would give very similar results as model A. Due to the more complicated relationship between Ci and Mw(v) in the acceleration case, a second order polynomial was chosen as the functional form of h and thus through the least-squares method we estimated the parameters b, c and d according to: Ci = d·Mw2(v) + b·Mw(v) + c /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 46. norsem_lund

  The recent Bothnian Bay M4.1 earthquake: where, how and why? B. Lund1, M. Uski2, H. Shomali1, D. Buhcheva1, S. Amini1, J. Kortström2 1Dep. of Earth Sciences, Uppsala University, Sweden 2Institute of Seismology, Dep. of Geosciences and Geography, University of Helsinki, Finland On 19 March 2016 a magnitude 4.1 earthquake occurred in the Bothnian Bay, between northern Sweden /media/norsem/norsem_lund.pdf

• 47. Group-1_Scenarios-for-AWM

  example can be given by the low cost still flood risk adaptation by implementing early warning system. But there is one more suggestion dfor stakeholders to restrict infrastructure in the cities of Horsens. Fiva PhD Courses : Adaptive management in relation to climate change (august 22 2011 - august 26 2011) 2 / 3 R es e a r c h Flood f r equenc y a n d i n t ensi t y c o m m un i c a t /media/loftslag/Group-1_Scenarios-for-AWM.pdf

• 48. Kok_and_Veldkamp_editorial_ES-2011-4160

  Tengö, D. Timmer, and M. Zurek. 2007. Linking futures across scales: a dialog on multiscale scenarios. Ecology and Society 12(1): 17. [online] URL: http://www.ecolog yandsociety.org/vol12/iss1/art17/. Borgatti, S. P., and P. C. Foster. 2003. The network paradigm in organizational research: a review and typology. Journal of Management 29(6):991-1013. Brenner, N. 2001. The limits to scale /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 49. CES_D2.4_VMGO

  (a) annual maximum temperature (b) and annual minimum temperature (c) as simulated by the ensemble of 9 CMIP3 AOGCMs for 2046-2065 relative to 1980-1999. Units are K. Dots denote grid boxes for which signal-to-noise ratio is greater than 1. a) b) c) d) Fig.2 Same as in Fig.1 but for changes in heat (a) and cold (c) wave /media/ces/CES_D2.4_VMGO.pdf

• 50. IPPC-2007-ar4_syr

  average temperature change, the upper ranges of sea level rise for SRES scenarios shown in Table 3.1 would increase by 0.1 to 0.2m.13 {WGI 10.6, SPM} Table 3.1. Projected global average surface warming and sea level rise at the end of the 21st century. {WGI 10.5, 10.6, Table 10.7, Table SPM.3} Temperature change Sea level rise (°C at 2090-2099 relative to 1980-1999) a, d (m at 2090-2099 relative /media/loftslag/IPPC-2007-ar4_syr.pdf