81 results were found for t 당산타이≒‘dm080.com”✂당산오피✩당산OP❊당산건마 당산업소 당산OP.

Results:

• 61. VI_2014_005

  model errors discussed in the previous section, a model time-series of 2-m temperature or 10-m wind speed, Mi(t), interpolated to the i-th station location, can be linearly transformed such that the mean square error compared with the local station time-series is minimised. Generally, the corrected time-series is then given by M˜i(t) = ai Mi(t)+bi ; (2) where at each station location, the correction /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 62. 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

• 63. VI_2019_009

  the backscatter, caused by haze, fog, mist, virga, precipitation or clouds is measured and the signal strength versus height, is stored and processed. The time (t) needed for the short pulse to traverse the atmosphere from the transmitter of the ceilometer to a back-scattering cloud base and back to the receiver of the ceilometer is directly proportional to the backscattering height shown /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 64. 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

• 65. GA_2009_91A_4_Andreassen

  the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob- servations /media/ces/GA_2009_91A_4_Andreassen.pdf

• 66. 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

• 67. 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

• 68. 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

• 69. Milly_etal-2008-Stationarity-dead-Science

  Cooperation and Development, Paris, 2006). 2. R. H. Webb, J. L. Betancourt, U.S. Geol. Surv. Water- Supply Paper 2379, 1 (1992). 3. C. A. Woodhouse, S. T. Gray, D. M. Meko, Water Resour. Res. 42, W05415 (2006). 4. Intergovernmental Panel on Climate Change (IPCC), in Climate Change 2007: The Physical Science Basis, Contribution of Working Group (WG) 1 to the Fourth Assessment Report of the IPCC (AR4 /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 70. 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