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21 results were found for 군산어플[모든톡 uy454]모든톡 uy454 어플구글웹문서노출 어플사이트홍보문의☉어플인터넷홍보㊧어플구글1페이지광고 ず嬌 thousand.


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  • 11. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

    1). Over the same period, the average total number of people reported affected2 per decade rose by 1200%, from approximately 38 thousand to 480 thousand. Meanwhile, the total cost of reported damage3 doubled, from US$ 1.2 billion to US$ 2.4 billion (2006 prices), although this could partially be explained by a higher density or vulnerability of infrastructure and areas being used by humans. More /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
  • 12. Moellenkampetal_etal-2010

  • 13. 2010_003rs

    to “bookshelf” type faulting. In June 2000, two large earthquakes of magnitudes ML6.4 and ML6.5 struck in the SISZ, three and a half days and approximately 17 km apart. Seismicity greatly increased in all Southwest Iceland and during 2000, roughly nineteen thousand microearthquakes were recorded there. The aim of this research is to relocate the earthquakes using a double- difference relative /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
  • 14. VI_2009_013

    the installation of digital, automatic SIL (South Iceland Lowland) network in 1991 and totals nearly one thousand events. In comparison, during the 8 year period between 1978 and 1985 only 3 events were detected in Eyjafjallajökull by the analogue, single component Icelandic Seismograph Network (Einarsson and Brandsdóttir, 2000). Three main seismic swarms have been recorded in Eyjafjallajökull during /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf
  • 15. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

    many contexts (socio- logical pragmatism), and through ‘microsituations’. This theory is of relevance for understanding partnerships and stakeholder involvement processes. BN construction in- deed took place through microsituations, it happened at a number of stakeholder meetings in Havelse; a small groundwater catchment of 35 km2 in North Zealand with a few thousand inhabitants living in the area /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
  • 16. 2010_012rs

    through relative relocation of over 50 thousand manually located microearthquakes. A selection of representative events from this database is used to construct a library, against which all new events will be compared. The selection is made on the basis of small relative location error of events on already mapped faults and small absolute error of other events. Due to the requirement of near-real /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf
  • 17. VI_2009_012

    densely populated farmland containing a few small towns, exposing a few thousand people to the hazards of strong to severe Earth shaking. The WVZ is mostly uninhabited, but the proximity of the capital, Reykjavík, to the WVZ and the SISZ, however subjects tens of thousands of people to moderate effects of shaking. Major power-lines to the capital, telecommunications and roads are also /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf
  • 18. VI_2020_005

    ; Quante and Colijn, 2016). The global mean sea level rise of last century and early 21st century was fast (see table 1) and strong evidence suggest that the 20th century sea level rise rate is faster than in the previous two thousand years (Church, Clark, et al., 2013). It is estimated to have been 1.7 0.2 mm/yr from 1901-2010, resulting in 19 (17-21) cm global mean sea level rise in the period /media/vedurstofan-utgafa-2020/VI_2020_005.pdf
  • 19. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  • 20. VI_2020_011_en

    it is considerably less well studied than on-land systems. The archipelago has formed over the last 70–120 thousand years and the currently visible features were produced during volcanic eruptions during the last 14–20 ka (Höskuldsson et al., 2013). There are currently between 15–18 islands and skerries and 45–75 submarine peaks (differing based on definition used while counting). In this work /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

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