47 results were found for gpt apisystem user(🏅xnseo.cc🏅)gpt apisystem user.TGX.

Results:

• 31. Climate and Modeling Scenarios

  4-5 Nov 2008, Helsinki, Finland. Kjellström, E. (2010). Deliverable 4.3. Report on user dialogue and analysis of regional climate scenarios for northern Europe. Swedish Meteorological and Hydrological Institute, Technical report, final version delivered 15 April 2010. Kjellström, E., Drews, M., Christensen, J. H., Haugen, J. E., Haakenstad, H. & Shkolnik, I. (2010). An ensemble of regional /ces/publications/nr/1680

• 32. Hare-2011-ParticipatoryModelling

  decision-making (see Squires and Renn in this issue). Model Type This refers to the type of model to be built as a result of the participatory modelling process. The categories are: • simulation model – a computational model of a system which allows the user to simulate system behaviour; • conceptual model – a model that qualitatively explains a system ‘on the basis of preconceived notions of how /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 33. ces-glacier-scaling-memo2009-01

  group how area changes are divided between the lowest elevation cell and higher cells. By de- fault the model adjusts the coefficient so that an estimate of the response time agrees with an estimate specified by the user in the initial glacier group file glacier-group-file0. -r rrv Relative remaining volume when to stop updating the coefficient k. When the volume of a glacier group has been /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 34. VI_2020_004

  ) ................. 89 Figure 61 Tephra accumulation rate on the ground on 8 October 1982 (Öræfajökull) ............ 90 Figure 62 Tephra accumulation rate on the ground in Skaftafell (Öræfajökull) ...................... 91 Figure 63 Preliminary intersectional map ................................................................................ 93 Figure 65 Initial user-interface of the public web-site /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 35. ces-oslo2010_proceedings

  other publications) and the user friendliness of the material, and  Suggestions for improvement for a future research programme, i.e. suggestions for an improved stakeholder relevance, dialogue and communication. One result from the stakeholder dialogue is that the CES project deals with very relevant issues that may considerably affect the energy sector. However, the potential effects /media/ces/ces-oslo2010_proceedings.pdf

• 36. Refsgaard_etal-2007-Uncertainty-EMS

  the model. Usually, the model is run within a graphical user interface (GUI) where many tasks have been automated.  STEP 4 (calibration and validation). This step is con- cerned with the process of analysing the model that was constructed during the previous step, first by calibrating the model, and then by validating its performance against independent field data. Finally, the reliability of model /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 37. 2011_005

  the database and user groups should be able to query the database, through an interface, e.g. a website or client program. Detailed equipment listing can be found in Appendix II. 11 2.3 Receivers Out of 63 CGPS stations that have been in the daily download routine since the beginning of the year, about 67% currently use Trimble NetRS receivers. Septentrio receivers are used in the NICE /media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf

• 38. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  elements of both natural system understanding and new technological developments. Finally, IWRM functions include: (3) financing functions and mechanisms including items such as national and local capital markets and mechanisms like grants and internal sources, user payments, subsidies, loans and equity capital. The main source of uncertainty here is related to the future societal developments /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 39. VI_2020_008

  values extracted from the time- series are not limited by their year of occurrence. However, the user must instead ensure independency of values and define a suitable threshold. In general, values in meteorological timeseries are dependent but, by declustering the data with a suitable minimum time window, the remaining values can be assumed approximately independent. For Icelandic conditions /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 40. 2010_016

  /media/ces/2010_016.pdf