58 results were found for 뉴욕『WWW,88M,KR』WWW,88M,KR 오킨스전자 에이티테크놀러지◥에머슨퍼시픽⒨아스타 ち肳 objective.

Results:

• 41. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  at e (C limat e models ) GC M s X X XX X X X X RCM s X X XX X X X X Initia lco n ditions / nat ura lva riabilit y X X XX X D ow ns ca lin g/ sta tis tic al co rr ec tio n X X X X X X X X X W ate r syst em impact s (H yd ro -e co lo gi ca lm o de ls) X X X X X XX X X X X X X X X X Socio -econo m ic imp act s (So ci o- ec on om ic to ol s) X X X X X X X X X XX X X X A da pt ati on m ea su re s X X X X /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 42. Daniell_etal-2010

  /media/loftslag/Daniell_etal-2010.pdf

• 43. VI_2014_001

  6 0 20 40 60 80 10 0 12 0 14 0 −ln(−ln(1−1/T)) Q( T) (m ?s) 1 2 5 10 20 50 100 T (years) l Obs. WaSiM vhm51 heM 95?bh ??Obs 95?bh ??W aSiM 95?bh heM Annual max. Q : GEV Distributions for vhm51 Index flood model no. 6 l l l l l l l l l l l l l l l l l l −2 0 2 4 6 0 50 10 0 15 0 −ln(−ln(1−1/T)) Q( T) (m ?s) 1 2 5 10 20 50 100 T (years) l Obs. WaSiM vhm52 heM 95?bh Obs 95?bh /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 44. vonKorff_etal-2010

  bodies of management, decision-support, risk, and participation literature. d’Aquino (2008) Patrick d’Aquino relies on 20 years of implementation and evaluation experience, mostly in a natural resource management context and in developing countries. His approach is, at this point, the least conceptually developed design method of the guides presented here, although it is linked to a theoretical /media/loftslag/vonKorff_etal-2010.pdf

• 45. VI_2014_006

  0 0 20 12 % Grassland <1 43 25 10 25 % Woodland <1 0 0 2 2 % Moss 59 25 0 14 13 % Little or no vegetation 35 27 30 63 36 % Wetland 0 5 46 6 7 % Lakes 6 <1 <1 <1 3 300 400 500 600 700 800 30 0 40 0 50 0 60 0 70 0 km km 2400 2200 2000 1800 1600 1400 1200 1000 800 600 400 200 0 m.a.s.l Watershed Glacier vhm19 vhm10 vhm26 vhm64 vhm66 Figure 1. Topography of Iceland and location of the watersheds /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 46. Bárðarbunga 2014 - October events

  Seismicity is similar to previous days: - There is low activity in the dyke intrusion. Around 20 earthquakes have occurred during the last 24 hours, all within magnitude 1.5 and in the northern part of the intrusion between the eruption site and to the south some kilometers under Dyngjujökull glacier. - About 80 earthquakes were detected on the caldera rim of Bárðarbunga. The largest earthquakes /earthquakes-and-volcanism/articles/nr/3011

• 47. Bardarbunga-2014_October-events

  the monthly articles give an overview of events: August, September, October, November, December, January, February and the current update. Calendar Below is a calendar with a short-cut to each day of this month's events: Oct.: 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 Panoramic view towards the eruptive site in Holuhraun 3rd September 2014. Photo /media/jar/Bardarbunga-2014_October-events.pdf

• 48. VI_2021_008

  providing 11 minutes of warning time before the eruption. The tremor signal emanating from Hekla travels outwards in a radial pattern, starting at stations closest to Hekla and then traveling outwards towards the borders of Iceland. Figure 8 shows the tremor amplitude plots for stations with a NE bearing from Hekla (Figure 8a) and a WSW bearing from Hekla (Figure 8b). Figure 9 shows /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 49. Bárðarbunga 2014 - October events

  Seismicity is similar to previous days: - There is low activity in the dyke intrusion. Around 20 earthquakes have occurred during the last 24 hours, all within magnitude 1.5 and in the northern part of the intrusion between the eruption site and to the south some kilometers under Dyngjujökull glacier. - About 80 earthquakes were detected on the caldera rim of Bárðarbunga. The largest earthquakes /earthquakes-and-volcanism/articles/nr/3011/

• 50. VI_2015_007

  0.95 vhm149 1.46 vhm205 1.01 vhm206 1.28 vhm221 0.9 vhm265 1.16 vhm277 0.87 vhm278 -0.12 18 l l l l l llll l llll lll ll lll lllll lllll ll l l l l l l l l l l l −2 0 2 4 6 0 1 2 3 4 −ln(−ln(1−1/T)) Q/ E[ Q] 1 2 5 10 20 50 100 T (years) l l l l l l l l vhm148 vhm149 vhm205 vhm206 vhm221 vhm265 vhm277 vhm278 Regional +/− 95% CI H1 0.995 H2 −0.877 l l l l l l l l l l l l l l l l l l l l l l l /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf