40 results were found for 【K528.COM】探探账号22级自用号 16anl.

Results:

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

  and HoSp 2002–2003 are shown. Fig. 7. (A) Late summer ice surface velocity determined by cross- correlation of 2.5 m resolution SPOT5 HRG satellite images ac- quired on 27 August and 22 September 2002. The numbers 1–3 point out locations where annual surface velocity signal could be deduced by correlating two SPOT5 HRG satellite images from late September 2002 and 2003 (see Table 2). (B–C) Depth /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 12. Hare-2011-ParticipatoryModelling

  Dispatch: 02.08.11 CE: E E T 5 9 0 No. of Pages: 19 ME: 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 Another possible driving force behind its popularity is changing legislation requiring environmental managers and policy-makers to increase stakeholder participation in their work [e.g /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 13. GA_2009_91A_4_Andreassen

  the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob- servations /media/ces/GA_2009_91A_4_Andreassen.pdf

• 14. 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

• 15. 2010_005_

  scenarios for Iceland, the full set of 22 GCM runs was reduced to those ten models, that performed best for SAT during the 1958–98 control period, compared with the ERA-40 reanalyses. The performance of individual GCMs was measured by determining the root-mean-squared deviations from ERA-40 reanalyses of annual spatial mean values of SAT within the study domain. This selection procedure resulted /media/ces/2010_005_.pdf

• 16. 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

• 17. VI_2019_009

  automatic record). ............. 19 11 Automatic records as a function of manual observations, where manual obser- vations over 20 km are not included. .......................................................... 20 12 Automatic records as a function of manual observations. ................................ 20 13 Frequency of present weather (SYNOP codes) observed by both stations. .......... 22 14 /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 18. Isskyrsla_20100116

  °26,8‘N – 21°55,0‘V 5. 66°26,5‘N – 22°00,7‘V 6. 66°25,8‘N – 22°00,7‘V 7. 66°27,5‘N – 22°03,5‘V 8. 66°27,2‘N – 22°07,4‘V 9. 66°28,0‘N – 22°11,1‘V 10. 66°27,0‘N – 22°12,5‘V 11. 66°26,2‘N – 22°14,0‘V 12. 66°25,5‘N – 22°14,7‘V 13. 66°26,6‘N – 22°19,4‘V Ísrönd var næst landi: 17,5 sjm. A af Horni. 12,5 sjm. N af Drangaskeri. 16 sjm. NNA af Þaralátursnesi. Veður: NA 20-35 hnútar og rigning, skýjafar fór /media/hafis/skyrslur_lhg/Isskyrsla_20100116_rett.pdf

• 19. 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

• 20. Reykholt-abstracts

  ), UK 19 Eric Lutz Department of Earth Sciences, Dartmouth College, USA 20 Hans-Gerd Maas Inst. of Photogrammetry and Remote Sens., TU Dresden, Germany 21 Eyjólfur Magnússon Institute of Earth Sciences (IES), University of Iceland 22 Ingvar Matthíasson National Land Survey of Iceland 23 Kjetil Melvold Norwegian Water Resources and Energy Directorate (NVE) 24 Finnur Pálsson Institute of Earth /media/vatnafar/joklar/Reykholt-abstracts.pdf