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

Results:

• 51. Kok_JGEC658_2009

  it will be one of the main aspects of this paper. 2.3. Properties The elements of a Fuzzy Cognitive Map are as follows:  Concepts: C1, C2, . . ., Cn. These represent the drivers and constraints that are considered of importance to the issue under consideration.  State vector: A = (a1, a2, . . ., an), where ai denotes the state of the node Ci. The state vector represents the value of the concepts /media/loftslag/Kok_JGEC658_2009.pdf

• 52. Reykholt-abstracts

  Lidar measurements of the cryosphere Reykholt, Iceland, June 20–21, 2013 Lidar measurements of the cryosphere Reykholt, Iceland, June 20–21, 2013 Abstract volume Lidar map of the ice-covered stratovolcano Öræfajökull in S-Vatnajökull, S-Iceland, surveyed by TopScan GmbH in August 2011 Lidar measurements of the cryosphere /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 53. 2010_003rs

  A (A1, A2, A3). ........................................................................................... 89 Figure B.2. Rake distribution for mapped faults/clusters in box B, Fagradalsfjall-W. ...... 90 Figure B.3. Rake distribution for mapped faults/clusters in box C, Fagdaralsfjall-E. ....... 90 Figure B.4. Rake distribution for mapped faults/clusters in box D, Kleifarvatn /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 54. 2010_012rs

  thus enabling the delineation of active faults in near-real time. Foreshocks preceding a large earthquake by more than 20 minutes will already have been located with high precision before the main shock occurs, and may already have delineated the fault plane of the coming main shock, thus allowing its faulting mechanism to be immediately inferred. Due to its size, the main shock /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 55. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  pm en t. Co ntex t(natura l,techni ca l an d so ci al sy ste m s): tra ns bo un da ry iss ue s w ith man y di ffe ren tspa tia lsc ales . So ci o ec o n o m ic an d cl im at e chang e ar e imp ortan t 1:Ont ologica l2:Sce nari o O fte n domina nt D ominant :Compl ex Int egrate d Sy ste m A na ly sis (C ISA ): in te gr at ed m o de lli ng an d as se ss m en tf or ex am in at io n o f co m pl ex re /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 56. VI_2013_008

  =1 day T=2 days T=3 days Statistics ME RMSE Q95–Q5 ME RMSE Q95–Q5 ME RMSE Q95–Q5 vhm 64 – method 1 6.8 48 130 13 82 215 14 101 269 vhm 64 – method 2 –2 35 97 –5.8 59 154 –9.4 84 204 vhm 64 – method 3 0.44 36 107 1.2 59 181 0.12 82 233 vhm 64 – method 4 –3.6 35 97 –6.7 57 154 –10 79 204 vhm 64 – persistence 0.03 53 / 0.02 86 / 0.05 103 / vhm 66 – method 1 1.4 15 33 1.9 21 48 1.5 23 53 vhm 66 /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 57. VI_2020_011_en

  –8% likelihood that a vent will open on Heimaey. In other words, there is a 92–97% likelihood that the next eruption within the volcanic system will not be on Heimaey. The most densely populated parts of Heimaey in the north and around the harbor are the most vulnerable to Moderate and Large lava flows originating on the island. Almost all infrastructure on the island is vulnerable to lava /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 58. IPPC-2007-ar4_syr

  of significant changes consistent with warming Percentage of significant changes consistent with warming 89%94%100% 100% 100% 100% 100% 100% 99%100%98% 96% 91% 94% 94% 90%90%92%94% 355 455 53 119 NAM LA EUR AFR AS ANZ PR* TER MFW** GLO 5 2 106 8 6 1 85 7650 120 24 7645 28,115 28,586 28,671 Changes in physical and biological systems and surface temperature 1970-2004 33 Topic 1 Observed changes /media/loftslag/IPPC-2007-ar4_syr.pdf