25 results were found for 九色丨反差91【搜占3k9M·CC】九色丨反差9120260115.qsd.

Results:

• 11. Kok_and_Veldkamp_editorial_ES-2011-4160

  ? Methodological reflections on scalar structuration. Progress in Human Geography 25:591-614. Bryan, B. A., N. D. Crossman, D. King, W. S. Meyer. 2011. Landscape futures analysis: assessing the impacts of environmental targets under alternative spatial policy options and future scenarios. Environmental Modelling and Software 26(1):83-91. Buizer, M., B. Arts, and K. Kok. 2011. Governance, scale /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 12. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  Thorbjarnardo´ttir B., Jakopsdo´ttir K. & Roberts M.J. 2010. Eruptions of Eyjafjallajo¨kull volcano, Iceland. Eos, Transac- tions of the American Geophysical Union 91, 190
  191. Hock R., de Woul M., Radic´ V. & Dyurgero M. 2009. Mountain glaciers and ice caps around Antarctica make a large sea-level rise contribution. Geophysical Research Letters 36, L07501, doi: 10.1029/2008GL037020. Hofmann-Wellenhof B /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 13. VI_2019_009

  /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 14. VI_2009_012

  /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 15. GA_2009_91A_4_Andreassen

  andEnergy Directorate (NVE), Oslo, Norway2Department of Geosciences, University of Oslo, Norway3Institute for Marine and Atmospheric Research, Utrecht University, Utrecht, the Netherlands Andreassen, L. and Oerlemans, J., 2009: Modelling long-term summer and winter balances and the climate sensitivity of Stor-breen, Norway. Geogr. Ann. 91 A (4): 233–251. ABSTRACT. Measurements of winter balance (bw /media/ces/GA_2009_91A_4_Andreassen.pdf

• 16. Kok_JGEC658_2009

  /media/loftslag/Kok_JGEC658_2009.pdf

• 17. Lorenzoni_Pidgeon_2006

  /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 18. VI_2020_004

  ) ................. 89 Figure 61 Tephra accumulation rate on the ground on 8 October 1982 (Öræfajökull) ............ 90 Figure 62 Tephra accumulation rate on the ground in Skaftafell (Öræfajökull) ...................... 91 Figure 63 Preliminary intersectional map ................................................................................ 93 Figure 65 Initial user-interface of the public web-site /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 19. 2010_003rs

  ................ 91 Figure B.5. Rake distribution for mapped faults/clusters in boxes E and F, Brennisteinsfjöll-Bláfjöll. ................................................................................. 92 Figure B.6. Rake distribution for mapped faults/clusters in box G, Ölfus. ......................... 93 Figure B.7. Rake distribution for mapped faults/clusters in box H, Hengill, active between January /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 20. VI_Arsskyrsla_2018_vef

  vatnsárunum 1979 til 1989 var meðalrennsli júnímánaðar 91 m3/s en á vatns- árunum 2008 til 2018 var það 71 m3/s. Þarna koma minni vorleys- ingar glöggt fram. Ef ársmeðalrennslið er skoðað er það 38 m3/s yfir fyrri áratuginn en 42 m3/s yfir seinni áratuginn. Þar fer munurinn í öfuga átt og rennslið hefur vaxið. Aukin úrkoma mælist nú á Norðurlandi og jöklar hafa rýrnað og skilað vatni. Tíminn sem /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf