eprintid: 6655 rev_number: 2 eprint_status: archive userid: 1 dir: disk0/00/00/66/55 datestamp: 2023-11-09 16:18:27 lastmod: 2023-11-09 16:18:27 status_changed: 2023-11-09 16:07:19 type: conference_item metadata_visibility: show creators_name: Batcha, S.R. creators_name: Sakidin, H. creators_name: Ahmad, A. title: Simpler Neill mapping function using nonlinear curve fitting method ispublished: pub note: cited By 0; Conference of 4th International Conference on Fundamental and Applied Sciences, ICFAS 2016 ; Conference Date: 15 August 2016 Through 17 August 2016; Conference Code:125141 abstract: For Neill mapping function,there are 26 mathematical operations for hydrostatic component and 11 operations for wet components need to be carried out in order to get the mapping function value. The Neill mapping function model for both hydrostatics and wet component are given in a form of continued fraction. In order to obtain fast results, the mapping function model need to be simplified. In this paper, the nonlinear curve fitting is used to simplify Neill Mapping Function model. Selection of model to be simplified is based on the model ability to reach mapping function value as low as 3 degree of elevation angle. To sum of error shows how close the simplified model result with the original model. The number of mathematical operation can be reduced after the process of simplification of the model. The percentage of reduction of operation for simplified model, especially for hydrostatic component is more than 80 percent. © 2016 Author(s). date: 2016 publisher: American Institute of Physics Inc. official_url: https://www.scopus.com/inward/record.uri?eid=2-s2.0-85005959361&doi=10.1063%2f1.4968062&partnerID=40&md5=63cc297d484ec413f03d50ae1e82908c id_number: 10.1063/1.4968062 full_text_status: none publication: AIP Conference Proceedings volume: 1787 refereed: TRUE isbn: 9780735414518 issn: 0094243X citation: Batcha, S.R. and Sakidin, H. and Ahmad, A. (2016) Simpler Neill mapping function using nonlinear curve fitting method. In: UNSPECIFIED.