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40 results were found for 【K528.COM】网易163邮箱批发 dxceo.


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  • 21. VI_2022_006_extreme

  • 22. 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
  • 23. CES_D2.4_task1

    NO +59:51:21 +10:26:12 163 P 2595 EIDSVOLL VERK NO +60:17:53 +11:09:47 181 P 2596 BJORNHOLT NO +60:03:03 +10:41:11 360 P 2597 KJELSAS I SORKEDALEN NO +60:02:13 +10:35:52 319 P 2598 MARIDALSOSET NO +59:58:08 +10:47:35 173 P 2599 NORDSTRAND NO +59:52:22 +10:47:33 118 P 2601 ATNSJOEN /media/ces/CES_D2.4_task1.pdf
  • 24. VI_2020_008

  • 25. 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
  • 26. IPPC-2007-ar4_syr

    (-33%) during 1970 to 2004 has been smaller than the com- bined effect of global income growth (77%) and global population growth (69%); both drivers of increasing energy-related CO2 emis- sions. The long-term trend of declining CO2 emissions per unit of en- ergy supplied reversed after 2000. {WGIII 1.3, Figure SPM.2, SPM} Differences in per capita income, per capita emissions and energy /media/loftslag/IPPC-2007-ar4_syr.pdf
  • 27. VI_2014_001

    vhm52 Kolka 163 688 1796 1957–1988 vhm92 Bægisá 39 934 1928 since 1966 vhm10 Svartá 398 535 813 since 1932 vhm45 Vatnsdalsá 456 553 846 since 1949 vhm200 Fnjóská 1096 715 1312 since 1976 vhm19 Dynjandisá 37 529 3018 since 1956 vhm38 Þverá 43 427 1761 since 1967 vhm204 Vatnsdalsá 103 456 2937 since 1977 vhm12 Haukadalsá 167 404 1773 since 1950 vhm198 Hvalá 195 403 1971 since 1976 8 vhm45 vhm12 /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf
  • 28. VI_2015_005

    This is also the case with cyclones in all three sectors. Cyclones in the eastern or western sector are also strongly affected by the presence of central cyclones. In both sectors, cyclones tend to move east, unless there are cyclones in the neighbouring sector, in which case pressure tendencies are reversed. 21 Figure 10. Composite mean temporal MSLP tendencies, for different MSLP modes. Com- posite mean /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
  • 29. VI_2015_009

    by rescaling a dimensionless regional flood frequency distribution or growth curve, qR(D;T ), com- mon to all sites of the homogeneous region, with the so-called index flood, µi(D), of the target site: bQi(D;T ) = µi(D)qR(D;T ); (1) where bQi(D;T ) is the estimated flood quantile, i.e. the T -year flood peak discharge averaged over duration D, at site i. The regional growth curve, qR(D;T /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
  • 30. Hare-2011-ParticipatoryModelling

    support ) Improv e mode l (integration) ; socia llea rnin g Farmers ,loca l aut horities , association s NO P IN D Cognitiv e mappin g HE T GM B NO P HE T Simulation - by-han d OT :Researcher s KA F F Iska r (Phas e1 ) Co n ce pt u al m o de l (D is cu ss io n su pp o rt ; Com m unication ) Improv e mode l (integration) ; socia llea rnin g Nationa l poli cy-maker s NO P IN D Cognitiv e mappin g HE /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

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