A global empirical model for estimating zenith tropospheric delay
Tropospheric delay acts as a systematic error source in the Global Navigation Satellite Systems (GNSS) position- ing. Empirical models UNB3, UNB3m, UNB4 and EGNOS have been developed for use in Satellite-Based Augmentation Systems (SBAS). Model performance, however, is limited due to the low spatial...
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description | Tropospheric delay acts as a systematic error source in the Global Navigation Satellite Systems (GNSS) position- ing. Empirical models UNB3, UNB3m, UNB4 and EGNOS have been developed for use in Satellite-Based Augmentation Systems (SBAS). Model performance, however, is limited due to the low spatial resolution of the look-up tables for meteoro- logical parameters. A new design has been established in this study for improving performance of the tropospheric delay model by more effectively eliminating the error produced by tropospheric delay. The spatiotemporal characteristics of the Zenith Tropospheric Delay (ZTD) were analyzed with findings that ZTD exhibits different annual variations at different locations and decreases exponentially with height increasing. Spherical harmonics are utilized based on the findings to fit the annual mean and amplitude of the ZTD on a global scale and the exponential function is utilized for height corrections, yielding the ZTrop model. On a global scale, the ZTrop features an average deviation of 1.0 cm and Root Mean Square (RMS) of 4.7 cm com- pared with the International GNSS Service (IGS) ZTD products, an average deviation of 0.0 cm and RMS of 4.5 cm compared with the Global Geodetic Observing System (GGOS) ZTD data, and an average deviation of -1.3 cm and RMS of 5.2 cm compared with the ZTD data from the Constellation Observing System of Meteorology, Ionosphere, and Climate (COSMIC). The RMS of the ZTrop model is 14,5% smaller than that of UNB3, 6.0% smaller than that of UNB3m, 16% smaller than that of UNB4, 14.5% smaller than that of EGNOS and equivalent to the sophisticated GPT2+Saas model in comparison with the IGS ZTD products. The ZTrop, UNB3m and GPT2+Saas models are finally evaluated in GPS-based Precise Point Positioning (PPP), as the models act to aid in obtaining PPP position error less than 1.5 cm in north and east components and relative large error (〉5 cm) in up component with respect to the random walk approach. |
doi_str_mv | 10.1007/s11430-015-5173-8 |
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Empirical models UNB3, UNB3m, UNB4 and EGNOS have been developed for use in Satellite-Based Augmentation Systems (SBAS). Model performance, however, is limited due to the low spatial resolution of the look-up tables for meteoro- logical parameters. A new design has been established in this study for improving performance of the tropospheric delay model by more effectively eliminating the error produced by tropospheric delay. The spatiotemporal characteristics of the Zenith Tropospheric Delay (ZTD) were analyzed with findings that ZTD exhibits different annual variations at different locations and decreases exponentially with height increasing. Spherical harmonics are utilized based on the findings to fit the annual mean and amplitude of the ZTD on a global scale and the exponential function is utilized for height corrections, yielding the ZTrop model. On a global scale, the ZTrop features an average deviation of 1.0 cm and Root Mean Square (RMS) of 4.7 cm com- pared with the International GNSS Service (IGS) ZTD products, an average deviation of 0.0 cm and RMS of 4.5 cm compared with the Global Geodetic Observing System (GGOS) ZTD data, and an average deviation of -1.3 cm and RMS of 5.2 cm compared with the ZTD data from the Constellation Observing System of Meteorology, Ionosphere, and Climate (COSMIC). The RMS of the ZTrop model is 14,5% smaller than that of UNB3, 6.0% smaller than that of UNB3m, 16% smaller than that of UNB4, 14.5% smaller than that of EGNOS and equivalent to the sophisticated GPT2+Saas model in comparison with the IGS ZTD products. The ZTrop, UNB3m and GPT2+Saas models are finally evaluated in GPS-based Precise Point Positioning (PPP), as the models act to aid in obtaining PPP position error less than 1.5 cm in north and east components and relative large error (〉5 cm) in up component with respect to the random walk approach.</description><identifier>ISSN: 1674-7313</identifier><identifier>EISSN: 1869-1897</identifier><identifier>DOI: 10.1007/s11430-015-5173-8</identifier><language>eng</language><publisher>Beijing: Science China Press</publisher><subject>Annual variations ; Atmospheric models ; Atmospheric sciences ; Earth and Environmental Science ; Earth Sciences ; EGNOS ; Global positioning systems ; GPS ; Ionosphere ; Meteorology ; Research Paper ; Troposphere ; 估计 ; 全球导航卫星系统 ; 对流层延迟 ; 平均偏差 ; 星基增强系统 ; 精密单点定位 ; 经验模型</subject><ispartof>Science China. Earth sciences, 2016-01, Vol.59 (1), p.118-128</ispartof><rights>Science China Press and Springer-Verlag Berlin Heidelberg 2015</rights><rights>Science China Press and Springer-Verlag Berlin Heidelberg 2016</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c446t-14d268efb10a935b5f7a6e7454a822b1a1e138749774064fc339a27a93bee4e73</citedby><cites>FETCH-LOGICAL-c446t-14d268efb10a935b5f7a6e7454a822b1a1e138749774064fc339a27a93bee4e73</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/60111X/60111X.jpg</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11430-015-5173-8$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11430-015-5173-8$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Yao, YiBin</creatorcontrib><creatorcontrib>Zhang, Bao</creatorcontrib><creatorcontrib>Xu, ChaoQian</creatorcontrib><creatorcontrib>He, ChangYong</creatorcontrib><creatorcontrib>Yu, Chen</creatorcontrib><creatorcontrib>Yan, Feng</creatorcontrib><title>A global empirical model for estimating zenith tropospheric delay</title><title>Science China. Earth sciences</title><addtitle>Sci. China Earth Sci</addtitle><addtitle>SCIENCE CHINA Earth Sciences</addtitle><description>Tropospheric delay acts as a systematic error source in the Global Navigation Satellite Systems (GNSS) position- ing. Empirical models UNB3, UNB3m, UNB4 and EGNOS have been developed for use in Satellite-Based Augmentation Systems (SBAS). Model performance, however, is limited due to the low spatial resolution of the look-up tables for meteoro- logical parameters. A new design has been established in this study for improving performance of the tropospheric delay model by more effectively eliminating the error produced by tropospheric delay. The spatiotemporal characteristics of the Zenith Tropospheric Delay (ZTD) were analyzed with findings that ZTD exhibits different annual variations at different locations and decreases exponentially with height increasing. Spherical harmonics are utilized based on the findings to fit the annual mean and amplitude of the ZTD on a global scale and the exponential function is utilized for height corrections, yielding the ZTrop model. On a global scale, the ZTrop features an average deviation of 1.0 cm and Root Mean Square (RMS) of 4.7 cm com- pared with the International GNSS Service (IGS) ZTD products, an average deviation of 0.0 cm and RMS of 4.5 cm compared with the Global Geodetic Observing System (GGOS) ZTD data, and an average deviation of -1.3 cm and RMS of 5.2 cm compared with the ZTD data from the Constellation Observing System of Meteorology, Ionosphere, and Climate (COSMIC). The RMS of the ZTrop model is 14,5% smaller than that of UNB3, 6.0% smaller than that of UNB3m, 16% smaller than that of UNB4, 14.5% smaller than that of EGNOS and equivalent to the sophisticated GPT2+Saas model in comparison with the IGS ZTD products. The ZTrop, UNB3m and GPT2+Saas models are finally evaluated in GPS-based Precise Point Positioning (PPP), as the models act to aid in obtaining PPP position error less than 1.5 cm in north and east components and relative large error (〉5 cm) in up component with respect to the random walk approach.</description><subject>Annual variations</subject><subject>Atmospheric models</subject><subject>Atmospheric sciences</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>EGNOS</subject><subject>Global positioning systems</subject><subject>GPS</subject><subject>Ionosphere</subject><subject>Meteorology</subject><subject>Research Paper</subject><subject>Troposphere</subject><subject>估计</subject><subject>全球导航卫星系统</subject><subject>对流层延迟</subject><subject>平均偏差</subject><subject>星基增强系统</subject><subject>精密单点定位</subject><subject>经验模型</subject><issn>1674-7313</issn><issn>1869-1897</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kD1PwzAQhi0EEhX0B7BFsLAYfP6Mx6riS6rEArPlpE6aKolTOx3Kr8dVKoQYuOVOuue9jxehGyAPQIh6jACcEUxAYAGK4fwMzSCXGkOu1XmqpeJYMWCXaB7jlqRgqUPVDC0WWd36wraZ64YmNGWqOr92bVb5kLk4Np0dm77OvlzfjJtsDH7wcdi4hGYJs4drdFHZNrr5KV-hz-enj-UrXr2_vC0XK1xyLkcMfE1l7qoCiNVMFKJSVjrFBbc5pQVYcMByxbVSnEhelYxpS1ViC-e4U-wK3U9zh-B3-3SZ6ZpYura1vfP7aEBJoZWkmiT07g-69fvQp-sSJZgWXEOeKJioMvgYg6vMENK34WCAmKOvZvLVJF_N0Vdz1NBJExPb1y78mvyP6Pa0aOP7epd0P5ukVJJwwin7Bhg8hDo</recordid><startdate>20160101</startdate><enddate>20160101</enddate><creator>Yao, YiBin</creator><creator>Zhang, Bao</creator><creator>Xu, ChaoQian</creator><creator>He, ChangYong</creator><creator>Yu, Chen</creator><creator>Yan, Feng</creator><general>Science China Press</general><general>Springer Nature B.V</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>~WA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M2P</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope></search><sort><creationdate>20160101</creationdate><title>A global empirical model for estimating zenith tropospheric delay</title><author>Yao, YiBin ; 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Earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Yao, YiBin</au><au>Zhang, Bao</au><au>Xu, ChaoQian</au><au>He, ChangYong</au><au>Yu, Chen</au><au>Yan, Feng</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A global empirical model for estimating zenith tropospheric delay</atitle><jtitle>Science China. Earth sciences</jtitle><stitle>Sci. China Earth Sci</stitle><addtitle>SCIENCE CHINA Earth Sciences</addtitle><date>2016-01-01</date><risdate>2016</risdate><volume>59</volume><issue>1</issue><spage>118</spage><epage>128</epage><pages>118-128</pages><issn>1674-7313</issn><eissn>1869-1897</eissn><abstract>Tropospheric delay acts as a systematic error source in the Global Navigation Satellite Systems (GNSS) position- ing. Empirical models UNB3, UNB3m, UNB4 and EGNOS have been developed for use in Satellite-Based Augmentation Systems (SBAS). Model performance, however, is limited due to the low spatial resolution of the look-up tables for meteoro- logical parameters. A new design has been established in this study for improving performance of the tropospheric delay model by more effectively eliminating the error produced by tropospheric delay. The spatiotemporal characteristics of the Zenith Tropospheric Delay (ZTD) were analyzed with findings that ZTD exhibits different annual variations at different locations and decreases exponentially with height increasing. Spherical harmonics are utilized based on the findings to fit the annual mean and amplitude of the ZTD on a global scale and the exponential function is utilized for height corrections, yielding the ZTrop model. On a global scale, the ZTrop features an average deviation of 1.0 cm and Root Mean Square (RMS) of 4.7 cm com- pared with the International GNSS Service (IGS) ZTD products, an average deviation of 0.0 cm and RMS of 4.5 cm compared with the Global Geodetic Observing System (GGOS) ZTD data, and an average deviation of -1.3 cm and RMS of 5.2 cm compared with the ZTD data from the Constellation Observing System of Meteorology, Ionosphere, and Climate (COSMIC). The RMS of the ZTrop model is 14,5% smaller than that of UNB3, 6.0% smaller than that of UNB3m, 16% smaller than that of UNB4, 14.5% smaller than that of EGNOS and equivalent to the sophisticated GPT2+Saas model in comparison with the IGS ZTD products. The ZTrop, UNB3m and GPT2+Saas models are finally evaluated in GPS-based Precise Point Positioning (PPP), as the models act to aid in obtaining PPP position error less than 1.5 cm in north and east components and relative large error (〉5 cm) in up component with respect to the random walk approach.</abstract><cop>Beijing</cop><pub>Science China Press</pub><doi>10.1007/s11430-015-5173-8</doi><tpages>11</tpages></addata></record> |
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subjects | Annual variations Atmospheric models Atmospheric sciences Earth and Environmental Science Earth Sciences EGNOS Global positioning systems GPS Ionosphere Meteorology Research Paper Troposphere 估计 全球导航卫星系统 对流层延迟 平均偏差 星基增强系统 精密单点定位 经验模型 |
title | A global empirical model for estimating zenith tropospheric delay |
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