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

Results:

• 51. Kok_JGEC658_2009

  input is often ad hoc and does not do justice to either the richness of the stories or the quantitative complexity of the models. The weak link between the qualitative and quantitative scenarios might well be the most problematic aspect of the Story-and-Simulation methodology. The main objective of this paper is to introduce, explain, and illustrate the potential of a possible improvement /media/loftslag/Kok_JGEC658_2009.pdf

• 52. Reykholt-abstracts

  /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 53. 2010_003rs

  distance between group centres DL Dalvík lineament EVZ Eastern volcanic zone fps fault plane solution GL Grímsey lineament GPS Global Positioning System HFF Húsavík-Flatey fault HM Hreppar micro-plate InSAR Interferometric Synthetic Aperture Radar J17 the 17 June large Holt earthquake J21 the 21 June large Hestvatn earthquake KR Kolbeinsey Ridge max48 maximum group size of 48 events NVZ /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 54. 2010_012rs

  J-17, J-21 and M-29. Locations of seismic stations are also sown (purple triangles). High-precision earthquake locations, with optimum achievable location accuracy on the order of tens of meters are currently obtained through relative relocation (double difference) of manually located earthquakes (Slunga et al., 1995; Hjaltadóttir and Vogfjörd, 2005). The objective is to obtain /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 55. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  strategies. The most effective form of AWRM employs management programmes that are designed to experimentally compare selected policies or practices, by evaluating alternative hypotheses about the system being managed (Pahl-Wostl 2007). The practised IWRM process itself is very dependent on the geographical, historical, cultural and economic context of a country or region. The objective of this paper /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 56. VI_2013_008

  /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 57. VI_2020_011_en

  are the objective of this report, but not for short-term immediate planning or evacuation during the first stages of an eruption. The main inputs of the MrLavaLoba code are topography, eruption volume and vent location. Lava does not flow like water and does not strictly follow the maximum downhill direction (steepest descent path), although topography, represented by a Digital Elevation Model (DEM /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 58. IPPC-2007-ar4_syr

  /media/loftslag/IPPC-2007-ar4_syr.pdf