91 results were found for Y アイリス〈ωωω,RTЗЗ,TOP〉コード:B77〉ミップスロット༿トラットfc🤞サッカートトサイト💛マカオベネシアン╜ソマリアの国家戦㍁パワーボールピクスター∿ジョージアサッカー␇プロトライブスコア∔.adq/.

Results:

• 71. 2010_016

  ............................................................................................................... 19 Table 4. Predicted quantitative changes from 1961–1990 to 2021–2050. ......................... 20 7 1 Abstract In order to investigate the effect of climate change on the hydrological regime in Iceland, future projections of river discharge were made for two watersheds with the WaSiM /media/ces/2010_016.pdf

• 72. VI_2020_004

  & Höskuldsson, 2008; Thordarson & Larsen, 2007). Highly active volcanic systems as Hekla, Katla, Bárðarbunga and Grímsvötn, have explosive eruptions rates of 82%, 97%, 90% and 95%, respectively (Gudmundsson & Larsen, 2016; Larsen & Gudmundsson, 2016b, 2016a; Larsen & Thordarson, 2016). Volcanic eruptions are quite common in Iceland and occur on average every two to five years (Larsen & Eiríksson /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 73. VI_2009_013

  striking westwards and a group of N-S-striking pressure axis dipping 45 degrees from the horizontal and more, suggesting that extensional forces play a large role. Figure 9 includes the mechanisms of 82 out of the 99 earthquakes in total located between 17 and 26 km depth and thus shows nearly the same results as described earlier for that interval, that the tension axis is chiefly horizontal /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 74. VI_2014_005

  ......................... 17 8 Monthly averages of SURFEX or projected 2-m air temperature ...................... 18 9 Local correction factors for 10-m wind speed ............................................... 19 10 Interpolated correction factors for 10-m wind speed ...................................... 20 11 Monthly averages of original or corrected temperature and wind speed .............. 21 12 /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 75. VI_2015_006

  cover. At night, the differences between land and ocean are small. However, during the day, especially with clear skies, as the land heats up faster than the surrounding water, the terrestrial longwave radiation losses can exceed those over the nearby cloud-free ocean by up to 80 W m 2. The total radiation received by the Earth’s surface is determined by factors that oppositely af- fect the short /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 76. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  Journal of Environmental Management 88 Heid , Øste d e A broad range of tools are available for integrated water resource management (IWRM). In the EU research project NeWater, a Human dependence on water leaves us vulnerable to climate change, flood and drought hazards, and poverty dynamic element of vulnerable groups and their relation- ship to water resources, and to represent the decisions /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 77. 2010_005_

  for Iceland were made. The CE project used an ensemble of six GCMs and RCMs from the PRUDENCE project for four different emissions scenarios (B1, B2, A2, and A1FI) developed by the Intergovernmental Panel on Climate Change (IPCC). The GCMs used by the CE project showed more warming during winter than summer. During winter, the median projected warming from 1961–90 to 2070–99 ranged from 3–6 K, and from 2 /media/ces/2010_005_.pdf

• 78. VI_2009_012

  Distance corrected PGV. ......................... 14  Figure 3. Corrected magnitudes, Mw(v) plotted against log distance.. .................................. 17  Figure 4. Magnitude estimates as a function of Ci. ................................................................ 18  Figure 5. Observed/predicted PGV residuals for each station. .............................................. 20  Figure 6 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 79. VI_2015_005

  depression .. 18 9 Relative seasonal occurrence of mean sea level pressure modes........................ 20 10 Composite mean temporal tendencies of mean sea level pressure...................... 22 11 Composite mean 500 hPa geopotential height anomalies ................................ 25 12 Composite mean surface wind speed anomalies ............................................ 27 13 Composite /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 80. CES_D2.4_task1

  about 20-25% in 2010 to about 50% in 2050. Perhaps surprisingly, a particularly high probability is found in Iceland, most likely as a result of the small 12 interannual variability there. As expected, the probability of very warn years rises even faster than that of warm months – in northern Europe from typically 30-40% in 2010 to about 60- 80% in 2030 and to 85-95% or even more in 2050 /media/ces/CES_D2.4_task1.pdf