MENG Lingpo, WU Jie, Yuan Yishuang. Receiver Autonomous Integrity Monitoring Based on Differential Carrier Phase[J]. Geomatics and Information Science of Wuhan University, 2011, 36(3): 271-275.
Citation: MENG Lingpo, WU Jie, Yuan Yishuang. Receiver Autonomous Integrity Monitoring Based on Differential Carrier Phase[J]. Geomatics and Information Science of Wuhan University, 2011, 36(3): 271-275.

Receiver Autonomous Integrity Monitoring Based on Differential Carrier Phase

More Information
  • Received Date: January 07, 2011
  • Revised Date: May 29, 2013
  • Published Date: March 04, 2011
  • We propose a new integer ambiguity resolution method,which enables one to determine DD carrier phase integer ambiguities at single epoch on the fly.Then receiver autonomous integrity monitoring(RAIM) based on carrier phase is researched.Test statistic is constructed using the method of least squares to test the integer ambiguity.Relationship between protection level,satellite geometry and miss detection probability is analyzed.Experiment results indicate that the success rate of integer ambiguity is 100% at single epoch on the fly.By adding one observation satellite,the vertical protection level will reduce about 0.2 m,the test statistic can detect cycle slips with 100% success rate.
  • Related Articles

    [1]HE Yuefan, NIE Guigen, WU Shuguang, LI Haiyang, LIAO Mi, GUO Yu. Analysis of Relationship Between CMONOC Coordinate Time Series Considering Rainfall and Hydrological Loading Under ITRF2014 Framework[J]. Geomatics and Information Science of Wuhan University, 2024, 49(6): 960-969. DOI: 10.13203/j.whugis20220042
    [2]WANG Yong, LIU Xiao, LIU Yanping, ZHAN Wei. MODIS PWV Correction Based on CMONOC and Regional Function Model[J]. Geomatics and Information Science of Wuhan University, 2023, 48(2): 224-231. DOI: 10.13203/j.whugis20200183
    [3]CHEN Junping, WANG Jungang, WANG Jiexian, TAN Weijie. SHAtrop: Empirical ZTD Model Based on CMONOC GNSS Network[J]. Geomatics and Information Science of Wuhan University, 2019, 44(11): 1588-1595. DOI: 10.13203/j.whugis20170384
    [4]GU Guohua, WANG Wuxing. Crustal Motions Observed from GPS Observations for the M6.9 Earthquake in Hawaii and the Eruption of the Kilauea Volcano in 2018[J]. Geomatics and Information Science of Wuhan University, 2019, 44(8): 1191-1197, 1204. DOI: 10.13203/j.whugis20180463
    [5]GU Guohua, WANG Wuxing. Results of GPS Observations for M7.8 Earthquake in 2016 in New Zealand and Discussion on Elastic Rebound Model[J]. Geomatics and Information Science of Wuhan University, 2017, 42(11): 1673-1680. DOI: 10.13203/j.whugis20170286
    [6]GU Guohua, WANG Wuxing, ZHAN Wei, LIANG Hongbao, ZHU Shuang. Preseismic, Coseismic and Postseismic Horizontal Crustal Movements of the Mw9.0 Tohoku Earthquake in Japan, 2011[J]. Geomatics and Information Science of Wuhan University, 2015, 40(12): 1669-1676. DOI: 10.13203/j.whugis20130744
    [7]LOU Junping, CHEN Kejie, LI Min, LI Wenwen. CMONOC Fiducial Station Deformation Before and Afterthe Tohoku-Oki Earthquake[J]. Geomatics and Information Science of Wuhan University, 2014, 39(1): 56-59.
    [8]XU Caijun, HE Ping, WEN Yangmao, ZHANG Lei. Coseismic Deformation and Slip Distribution for 2011 Tohoku-Oki Mw 9.0 Earthquake:Constrained by GPS and InSAR[J]. Geomatics and Information Science of Wuhan University, 2012, 37(12): 1387-1391.
    [9]SHEN Fei, LI Jiancheng, GUO Fei. Analysis of the Coseismic Displacements Along Eastern Coast of China Caused by the 2011 Tohoku-Oki Earthquake Using Epoch-by-Epoch PPP[J]. Geomatics and Information Science of Wuhan University, 2012, 37(11): 1345-1347.
    [10]YANG Shaomin, NIE Zhaosheng, JIA Zhige, PENG Maolei. Far-field Coseismic Surface Displacement Caused by the Mw9.0 Tohoku Earthquake[J]. Geomatics and Information Science of Wuhan University, 2011, 36(11): 1336-1339.

Catalog

    Article views (1320) PDF downloads (435) Cited by()
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return