Simpler UNBabc Mapping Function for Global Positioning System (GPS) Tropospheric Delay

The UNBabc(E) mapping function models should be simplified to allow faster calculation and also better understanding of the models. Many modern mapping function models use mapping functions in the form of continued fractions which is quite tedious in calculation. There are 11 mathematical operation...

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محفوظ في:
التفاصيل البيبلوغرافية
المؤلفون الرئيسيون: Sakidin, Hamzah, Tay, Choo Chuan
التنسيق: Conference or Workshop Item
اللغة:English
منشور في: 2010
الموضوعات:
الوصول للمادة أونلاين:http://eprints.utem.edu.my/id/eprint/4879/1/Proceedings_of_ICEI_2010.pdf
http://eprints.utem.edu.my/id/eprint/4879/
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id my.utem.eprints.4879
record_format eprints
spelling my.utem.eprints.48792015-05-28T03:29:05Z http://eprints.utem.edu.my/id/eprint/4879/ Simpler UNBabc Mapping Function for Global Positioning System (GPS) Tropospheric Delay Sakidin, Hamzah Tay, Choo Chuan Q Science (General) The UNBabc(E) mapping function models should be simplified to allow faster calculation and also better understanding of the models. Many modern mapping function models use mapping functions in the form of continued fractions which is quite tedious in calculation. There are 11 mathematical operations for UNBabc(E) to be carried out before getting the mapping function scale factor. The mapping functions for UNBabc(E) models for hydrostatic and non hydrostatic components are given in a form of continued fraction are to be simplified. UNBabc(E) mapping function models are selected due to its ability to calculate mapping function value down to 2 degree of elevation angle. By using linear, hyperbolic, logarithm and also regression method, the mapping function models can be simplified and at the same time can produce the same result. The calculation of sum of errors shows that the deviation of the simplified models from the original models is not significant. The computation time between the original model and simplified model shows that the simplified UNBabc(E) model is 6.5 times faster than the original model for both hydrostatic and non hydrostatic component. As the coefficient of zenith hydrostatic delay and also zenith non hydrostatic delay, the mapping function scale factor value plays an important role for getting the total tropospheric delay value. 2010 Conference or Workshop Item PeerReviewed application/pdf en http://eprints.utem.edu.my/id/eprint/4879/1/Proceedings_of_ICEI_2010.pdf Sakidin, Hamzah and Tay, Choo Chuan (2010) Simpler UNBabc Mapping Function for Global Positioning System (GPS) Tropospheric Delay. In: The 2nd International Conference on Engineering and ICT,2010, Melaka, Malaysia, 18-20 February, 2010, Holiday Inn, Melaka, Malaysia.
institution Universiti Teknikal Malaysia Melaka
building UTEM Library
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Teknikal Malaysia Melaka
content_source UTEM Institutional Repository
url_provider http://eprints.utem.edu.my/
language English
topic Q Science (General)
spellingShingle Q Science (General)
Sakidin, Hamzah
Tay, Choo Chuan
Simpler UNBabc Mapping Function for Global Positioning System (GPS) Tropospheric Delay
description The UNBabc(E) mapping function models should be simplified to allow faster calculation and also better understanding of the models. Many modern mapping function models use mapping functions in the form of continued fractions which is quite tedious in calculation. There are 11 mathematical operations for UNBabc(E) to be carried out before getting the mapping function scale factor. The mapping functions for UNBabc(E) models for hydrostatic and non hydrostatic components are given in a form of continued fraction are to be simplified. UNBabc(E) mapping function models are selected due to its ability to calculate mapping function value down to 2 degree of elevation angle. By using linear, hyperbolic, logarithm and also regression method, the mapping function models can be simplified and at the same time can produce the same result. The calculation of sum of errors shows that the deviation of the simplified models from the original models is not significant. The computation time between the original model and simplified model shows that the simplified UNBabc(E) model is 6.5 times faster than the original model for both hydrostatic and non hydrostatic component. As the coefficient of zenith hydrostatic delay and also zenith non hydrostatic delay, the mapping function scale factor value plays an important role for getting the total tropospheric delay value.
format Conference or Workshop Item
author Sakidin, Hamzah
Tay, Choo Chuan
author_facet Sakidin, Hamzah
Tay, Choo Chuan
author_sort Sakidin, Hamzah
title Simpler UNBabc Mapping Function for Global Positioning System (GPS) Tropospheric Delay
title_short Simpler UNBabc Mapping Function for Global Positioning System (GPS) Tropospheric Delay
title_full Simpler UNBabc Mapping Function for Global Positioning System (GPS) Tropospheric Delay
title_fullStr Simpler UNBabc Mapping Function for Global Positioning System (GPS) Tropospheric Delay
title_full_unstemmed Simpler UNBabc Mapping Function for Global Positioning System (GPS) Tropospheric Delay
title_sort simpler unbabc mapping function for global positioning system (gps) tropospheric delay
publishDate 2010
url http://eprints.utem.edu.my/id/eprint/4879/1/Proceedings_of_ICEI_2010.pdf
http://eprints.utem.edu.my/id/eprint/4879/
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