81 results were found for t 오피나라ⓠ《optop5.com〕 오피나라 오피나라 오피나라 오피나라.

Results:

• 61. Reykholt-abstracts

  to get highly accurate results in photogrammetric processing of historical photographs. REFERENCE Jóhannesson, T., H. Björnsson, F. Pálsson, O. Sigurðsson and Þ. Þorsteinsson. 2011. Lidar mapping of the Snæfellsjökull ice cap, western Iceland, Jökull, 61,19–32. Lidar measurements of the cryosphere Reykholt, Iceland, June 20–21, 2013 12 Csatho and others The ICESat-2 mission: design /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 62. Comparison of displacement velocities for different time periods

  /about-imo/news/nr/3074

• 63. Mid-Latitudes-Agenda1_nov2013EH

  Agenda *All presentations will be in the Forgardur (forecourt) underground basement room of the IMO building at Bustadavegur 7, unless otherwise noted. Wednesday, 13 November Time Agenda Item 09:00 – 09:15 Welcome and Introductions - T Jónsson and E Hanna 09:15 – 09:30 Meeting Structure and Overview - J Overland and E Hanna 09:30 – 10:40 09:30 – 09:45 09:45 – 10:05 10:05 – 10:25 /media/loftslag/Mid-Latitudes-Agenda1_nov2013EH.pdf

• 64. Crochet_Philippe_CES_2010

  ≤   ≤ >− 0 00 0 )( TTif TTifTTDDFsnow   ≤ >− 0 00 0 )( TTif TTifTTDDFice Mean annual temperature difference Difference relative to 1971-2000 Difference between 25% warmest and 25% coldest years barb2right +1°C (25% warmest) barb2right -0.7°C (25% coldest) barb2right +1.7°C Catchment elevation (m.a.s.l) Catchment elevation (m.a.s.l) s n o w m e l t ( m m / d ) g l a c i a l m e l t /media/ces/Crochet_Philippe_CES_2010.pdf

• 65. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  in ty N at ur e o f u n ce rta in ty Inp ut dat a Mo de l Co ntex t Multi pl e knowl edg e fra m es Ambi guit y Ep istemi c un certaint y (re du cib le) Aleator y u n ce rta in ty (ir red uc ibl e) Pa ramete r val ue s Mode l techni ca l as pe ct s Mo de l st ru ct ur e G re en ho us e ga s em iss io ns X X X X X X X X X X Socio -econo m ic scena rio s X X X X X X X X X XX X X X Fu tu re cl im /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 66. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  su lta tio n o f st ak eh ol de rs, co m m en tin g an d o bje cti ng o n go al s an d tra ns bo un da ry as pe ct s (Ens erin k et al .200 3; Raa dgeve ran d Mos ter t200 5). Asse ssmen to fexi stin g situatio n D at a (na tu ra ls ys te m s): 1: Ep ist em ic O fte n do m in an t In te rn at io na lm o n ito rin g n et w or k se tu p, i.e .thr oug h IC PR .Su stainabl e tra ns bo un da ry co o pe /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 67. Perrels-CBA

  / design, availability, materials, ICT, modal split) 26.8.2011Adriaan Perrels/IL 5 Categorising stages of adaptation Passive Adaptation - automatic in nature and economy - only ex post measures (no anticipation) Active Adaptation - automatic in nature and economy - ex ante and ex post policies Emission scenario dependent baseline (A1-T, B1, A2, etc.) Reference costs and benefits /media/loftslag/Perrels-CBA.pdf

• 68. Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication

  on the real and tangible (“Sensing”, S) or by focusing on the big picture and the relationships between ideas (“Intuition”, N). The T/F dichotomy characterizes the processes people use to make decisions. Some prefer to make decisions based on objective, logical reasoning (“Thinking”, T), while others rely more on personal values and the impact of decisions on others (“Feeling”, F). Finally, the J/P /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 69. 2013_001_Nawri_et_al

  the validity of the ideal gas law, hydrostatic balance, a piecewise linear vertical gradient of air temperature, and neglecting the effects of water vapour. Pressure, p, as a function of height can then be derived through vertical integration of the hydrostatic balance equation, and is given by p(h(x;y);z) = p0 exp g R Z h(x;y)+z 0 dx T (x ) ; (5) where p0 is pressure at mean sea level, T /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 70. Kok_1-scenarios-lecture-1

  scale: The Hierarchy Theory • Emerged as part of a movement toward a general science of complexity • Rooted in various other disciplines but operationalised by ecologists in the 1970s and 1980s • Key references: Allen, T. F. H. and T. B. Starr. 1982. Hierarchy: perspectives for ecological complexity. University Chicago Press. Allen T. F. H. and T. Hoekstra. 1992. Toward a unified ecology /media/loftslag/Kok_1-scenarios-lecture-1.pdf