36 results were found for 竞技宝app下载安装平台-澳洲幸运10信誉平台-【✔️访问㊙️360bet.net✔️】-竞技宝app下载安装平台-澳门十大信誉平台排行榜-(✔️网址sogou7.com✔️)-竞技宝app下载安装平台-竞技宝app下载安装平台-竞技宝app下载安装平台-(✔️网址sogou7.com✔️).

Results:

• 11. Journal_of_Hydrology_Veijalainen_etal

  ) in Europe yield contradictory results on the changes in floods in many parts of Europe, including Finland. Dankers and Feyen (2008) reported a considerable reduction of 10–40% in 100-year discharges in Finland, much of northern Sweden and north-western Russia by the end of the century due to decrease in snow accumulation; however Lehner et al. (2006) evaluated that the 100-year floods in the same areas /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 12. VI_2020_005

  (Quante and Colijn, 2016). Work on risk analysis and adaptation is in different stages in the countries of the world. Coastal floods have caused problems in Iceland in the past (Jóhannsdóttir, 2017) and are likely to do so in the future as well. Large coastal floods can be expected in Iceland every 10 - 20 years and the probability of such events can rise with climate change (Almannavarnir, 2011 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 13. Adalgeirsdottir-etal-tc-5-961-2011

  were carried out to obtain the flow and sliding parameters for Hoffellsjökull that resulted in a good simulation of the observed 20th century evolution of the glacier geometry. The obtained values for the rate factor and the sliding parameter are A= 4.6× 10−15 s−1 kPa−3 and C = 10× 10−15 m a−1 Pa−3, respectively. The ice divide is kept at a fixed location in the model com- putations presented here /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 14. GA_2009_91A_4_Andreassen

  to highly negative summer balances, but also lower bw than the average for 1949–2006. Calculated change in specific mass balance for a ±1°C change in air tem- perature was ±0.55 m w.e., whereas a ±10 % in- crease in precipitation represented a change of ± 0.20 m w.e. Model results further indicated that for a 2°C warming, the ablation season will be extend- ed by c. 30 days and that the period /media/ces/GA_2009_91A_4_Andreassen.pdf

• 15. Paper-Olafur-Rognvaldsson_92

  a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 16. VI_2009_006_tt

  to theoretical framework. I do also want to thank him for an enjoyable time during this work, both in the office and in the field. This work was carried out as a part of the Skaftá cauldrons research project which was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja- sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com- pany), the National Energy /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 17. IPPC-2007-ar4_syr

  data, models or analyses, then the following scale of confidence levels is used to express the assessed chance of a finding being correct: very high confidence at least 9 out of 10; high confidence about 8 out of 10; medium confidence about 5 out of 10; low confidence about 2 out of 10; and very low confidence less than 1 out of 10. Where uncertainty in specific outcomes is assessed using expert /media/loftslag/IPPC-2007-ar4_syr.pdf

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

  The Netherlands 123 Reg Environ Change (2010) 10:263–284 DOI 10.1007/s10113-009-0108-6 On a global scale, the number of disasters caused by weather-related phenomena such as storms, floods, and droughts has more than doubled over the past decade, from 175 in 1996 to 391 in 2005 (IFRC 2008). The same trend (Fig. 1) is being observed in the case-studies under inves- tigation, which is Rivierenland /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 19. 2010_005_

  day during the 1961–90 control period, differences in percent of the control period between the control period and the 2021–50 reference period, and linear trends in percent of the control period per decade within the 2004–50 period, for the IPCC GCM ensemble mean, the SMHI-RCAO, the MetNo-HIRHAM, and the DMI-HIRHAM5. . . . . . . . . . . 31 10 Mean annual air pressure at mean sea level /media/ces/2010_005_.pdf

• 20. VI_2015_009

  ) vhm238 S O N D J F M A M J J A l l l l ll l lll l l l l l l l l l l l l l l l l l l l l 0 100 200 300 10 0 30 0 50 0 70 0 Days since Sept. 1st Q (m ³/s ) vhm144 S O N D J F M A M J J A l l l l l l l l l l l l ll l l l l l l l l l l l l l l ll l 0 100 200 300 10 0 20 0 30 0 40 0 Days since Sept. 1st Q (m ³/s ) vhm145 S O N D J F M A M J J A l l l l l l l l l l 0 100 200 300 10 0 20 0 30 0 40 0 /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf