89 results were found for X 정보이용료현금화 ≰ㅋr톡 1SEC≱ 티켓타카 Y 정보이용료현금화 전문 포탈 지난해🛤manoeuver/.

Results:

• 41. VAT_newsletter_2018_06

  Lifandi kennslu stofa í lolags breytingumA natural laboratory to study climate change Jöklar ÍslandsIcelandic glaciers Yrlit um íslenska jökla í árslok  Jöklar á Íslandi hafa hopað hratt í rúma tvo áratugi og er rýrnun þeirra einhver helsta aeiðing hlýnandi loslags hérlendis og skýr vitnis burð- ur um hlýn un ina. Hér er gerð stutt grein fyr ir breytingum á jökl un um síðan um aldamótin /media/Eplicanámskeið/VAT_newsletter_2018_06.pdf

• 42. NONAM_1st_workshop_summary_v3

  / administrative aggregation level. Table 1 – Tentative identification of relevant (predominant) operating levels. Local Regional National* International public privat e public privat e public privat e public privat e Infrastructure designers x x x XX X Infrastructure builders x x XX X Infrastructure operators x x x X X Transport service operators (freight; passengers /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 43. Cradden_Lucy_CES_2010

  Capacity (A) F r e q u e n c y control future +0.4std dev (as % of mean) -0.68max -8.32min -1.74mean % change June 2010 15 Time series 450 500 550 600 650 700 Hour C a p a c i t y ( A ) Typical year of control period Seasonal average rating Calculated capacity 450 500 550 600 650 700 Hour C a p a c i t y ( A ) Typical year under future scenario Calculated capacity Seasonal average /media/ces/Cradden_Lucy_CES_2010.pdf

• 44. VI_2022_006_extreme

  of the melt season as retrieved by the third filtering method. 15 4.1.2 Results For each catchment, all the dates retrieved by the last filter were stored in a table. These dates were then plotted together, as shown for four catchments in Figure 7. Results for the other catchments are included in Appendix I (Figures I.1 – 11). On each plot, the x-axis shows the 39 years used for the study /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 45. 2010_017

  ) storage coefficient of interflow ki; (3) drainage density d; (4) the fraction of surface runoff from snowmelt; and (5) the recession constant krec for the decreasing saturated hydraulic conductivity with increasing depth. For the groundwater flow, adjusted parameters (6–7) are the hydraulic conductivity in the X and Y direction. The hydraulic conductivity is adjusted in distributed grids unlike /media/ces/2010_017.pdf

• 46. norsem_michalek

  was deployed and together with the permanent NNSN stations in that area it contained 33+ stations within span 350 x 200 km. About 1250 earthquakes of M>0.0 was recorded during the project period and new map of seismicity of that area was retrieved. The main aim of the project is to reveal the stress field in that particular region and therefore determination of stable /media/norsem/norsem_michalek.pdf

• 47. ces_geus_paakitsoq_full_report

  of Geophysical Research, 108(D3), 4124, doi:10.1029/2002JD002287. IPCC (2001), Climate change 2001: the scientific basis. Contribution of working group I to the third assessment report of the intergovernmental panel on climate change. (eds. Houghton, J. T. , Y. Ding, D. J. Griggs, M. Noguer, P. J. van der Linden, X. Dai, K. Maskell and C. A. Johnson), Cambridge University Press, Cambridge, UK /media/ces/ces_geus_paakitsoq_full_report.pdf

• 48. Ice subsidence above eastern Skaftá cauldron

  This graph shows the ice-surface lowering (subsidence) of the eastern Skaftá ice-cauldron in Vatnajökull ice cap in October 2015. Vertical displacement (m) was monitored by near real time presentation of data from a GPS station, mounted in the middle of the cauldron. The maximum elevation above sea level, top left (hæð), refers to the zero value on the y-axis; while such value top right /hydrology/research/skafta-cauldron/

• 49. ces_SA_group_flyer_new

  by season (%) between 1991-2007 and 1961-1990 in the Baltic countries 1 9 0 0 1 9 2 0 1 9 4 0 1 9 6 0 1 9 8 0 2 0 0 0 - 1 5 - 1 0 - 5 0 5 1 0 1 5 P r e c i p i t a t i o n a n o m a l y ( % ) R e g i o n 1 R e g i o n 2 R e g i o n 3 R e g i o n 4 F un c t ion P lo t 5 1 9 0 0 1 9 2 0 1 9 4 0 1 9 6 0 1 9 8 0 2 0 0 0 - 1 . 5 - 1 - 0 . 5 0 0 . 5 1 1 . 5 T e m p e r a t u r e a n o m /media/ces/ces_SA_group_flyer_new.pdf

• 50. norsem_lindholm

  Neotectonics in Nordland; NEONOR 2 C. Lindholm, O. Olesen, I. Janutyte, S. Gradman, M. Keiding, H. Kierulf, M. Ask, J. Dehls, Y. Maystrenko, F. Riis, L. Rise and other project partners The Nordland shore region is known to be seismically active with deep local sediment basins on the continental shelf that stretches some 200 km west of the coastline. The offshore areas west of Nordland have /media/norsem/norsem_lindholm.pdf