30 results were found for 【K06.CC】无名AI-ChatGPT账号购买 ms8oj.

Results:

• 21. VI_2015_007

  distribution and parameter estimation method The Generalized Extreme Value (GEV) distribution (Jenkinson, 1955) was adopted to model the flood frequency distribution from the AMF series: Qi(D;T ) = ei + ai ki (1 [ ln(1 1=T )]ki) if ki 6= 0 ei ailn( ln(1 1=T )) if ki = 0 (7) where ei is the location parameter, ai is the scale parameter and ki is the shape parameter. The method of probability weighted /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 22. 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

• 23. Perrels-CBA

  enhanced weather effects on road infrastructure • traffic safety • road maintenance • traffic capacity • Assessing flood risks in cities • TOLERATE: From climate modeling to appraisal of counter measures • IRTORISKI: Extended event-tree analysis Next pages (EWENT) 26.8.2011Adriaan Perrels/IL 26 Road capacity effects of weather & CC Changes in the supply curve caused by extreme weather conditions /media/loftslag/Perrels-CBA.pdf

• 24. NONAM_1st_workshop_summary_v3

  -out group, assuming the initiative is at the public side. Red: inside transport system; blue: direct impact on size & quality of demand for road vehicle movements; grey: auxiliary services that strongly interact with effects of CC. Various possible effects of climate change on road infrastructure and its users The expected effects of a changing climate in Nordic countries imply among others /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 25. 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

• 26. VI_2020_004

  /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 27. 2010_003rs

  /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 28. Adalgeirsdottir-etal-tc-5-961-2011

  The Cryosphere, 5, 961–975, 2011 www.the-cryosphere.net/5/961/2011/ doi:10.5194/tc-5-961-2011 © Author(s) 2011. CC Attribution 3.0 License. The Cryosphere Modelling the 20th and 21st century evolution of Hoffellsjökull glacier, SE-Vatnajökull, Iceland G. Aðalgeirsdóttir1,2, S. Guðmundsson1, H. Björnsson1, F. Pálsson1, T. Jóhannesson3, H. Hannesdóttir1, S. Þ. Sigurðsson4, and E. Berthier5 /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 29. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 30. VI_2013_008

  [Q(t);Q(t 1);Q(t 2)] E[Q(ui);Q(ui 1);Q(ui 2)] , ai = Qb(t) Qb(ui) , bi = Q(t) Qb(t) Q(ui) Qb(ui) , and Qb(t) and Qb(ui) are baseflows calculated using the UKIH baseflow separation method (Piggott et al., 2005). All rescaling coefficients were limited to a minimum value of 0.25 and a maximum value of 5. 4.5 Deterministic prediction A deterministic forecast was derived from the ensemble by taking /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf