56 results were found for 99贵宾汇开户(3266-409-932薇Q).adw.

Results:

• 41. 2010_003rs

  ca ti o n s fo r th e la rg est e a rt h q u a ke s w it h in t h e S IS Z b et w ee n 1 7 0 6 a n d 2 0 0 8 d en o te d b y w h ite fil le d c ir cles. E stim a te d f a u lt p la n es o f h is to ric a l ea rt h q u a ke s a re s h o w n a s w h ite , th ick li n es ( fr o m R o th , 2 0 0 4 ). F a u lt p la n es f ro m 1 9 9 8 ( V o g fj ö rd et a l. , 2 /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 42. Dataseries and components

  -180 toxafen-26, -50, -62 BDE-47, -99, -100 Stórhöfði in the Westman Islands - foreign research: Continuous measurements of surface ozone. Ambient air: Instantaneous samples weekly using ~2 litre glass containers for atmospheric CO2, CH4, CO, H2, SF6 and N2O, as well as the C13 and O18 isotopes in carbondioxide and the C13 isotope in methane. For quality, a pair of identical samples are taken /pollution-and-radiation/pollution/components/

• 43. bb100days_ens

  opportunity ever to follow a caldera subsidence in Iceland with modern scientific measurements and methods. Number of earthquakes between 16 August 2014 00:00 and 09 December 2014 at 08:30 all intrusion caldera Kistufell Askja HB / HBT TFJ Kverkfj. automatic ~ 34.000 - - - - - - - checked ~ 17.500 ~ 7.500 ~ 7.000 ~ 120 ~ 340 ~ 1500 ~ 470 ~20 M3.0-3.9 836 99 721 6 2 3 4 1 M4.0-4.9 462 7 453 1 1 /media/jar/bb100days_ens.pdf

• 44. Dyrrdal_Anita_CES_2010

  : Significant at 90% CL Norwegian Meteorological Institute met.no Fokstugu (973 m.a.s.l.) Introduction Data & Methods Results Trends in start and end: Significant at 99% CL /media/ces/Dyrrdal_Anita_CES_2010.pdf

• 45. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  19 CMIP3 GCMs are used (Table 2.1). The horizontal grid spacing of these models varies from 1.1 q latitude × 1.1q longitude to 4 q latitude × 5q longitude. For each 2 Some of the RCM simulations in the ENSEMBLES data base were conducted with funding from other sources, including CES. 5 model, a 198-year time series (1901-2098) obtained /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

• 46. IPPC-2007-ar4_syr

  judgment and statistical analysis of a body of evidence (e.g. observations or model results), then the following likelihood ranges are used to express the assessed probability of occurrence: virtually certain >99%; extremely likely >95%; very likely >90%; likely >66%; more likely than not > 50%; about as likely as not 33% to 66%; unlikely <33%; very unlikely <10%; extremely unlikely <5 /media/loftslag/IPPC-2007-ar4_syr.pdf

• 47. Flood from Skaftá

  /about-imo/news/flood-in-estern-skafta

• 48. New article on glacier changes in

  An article recently published in the journal Frontiers in Earth Science on glacier changes in Iceland describes changes in the volume and mass of the Icelandic glaciers since they reached historical maximum extent at the end of the so-called Little Ice Age shortly before 1900. The results of a number of studies covering about 99% of the glacier area are summarized /about-imo/news/new-article-on-glacier-changes-in-iceland-over-the-past-130-years

• 49. Flood from Skaftá

  /about-imo/news/flood-in-estern-skafta/

• 50. Paper-Olafur-Rognvaldsson_91

  of Icelandic glaciers 1992–1997). Rep. OS-98082 (in Icelandic), National Energy Authority, Reykjavík. Sigurðsson, O., Thorsteinsson Th., Ágústsson S. M. and Einarsson B. 2004. Afkoma Hofsjökuls 1997–2004. (Mass balance of Hofsjökull 1997–2004.) Rep. OS-2004/029, National Energy Authority, Reykjavík. Uppala, S.M., and 45 co-authors 2005. The ERA-40 re-analysis. Q. J. R. Mete- orol. Soc., 131, 2961 /media/ces/Paper-Olafur-Rognvaldsson_91.pdf