验后平差法的应用

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主要介绍了海洋卫星在处理数据时的一种方法,是很好的处理交叉点的方法,对初学海洋数据分析人员来说,是入门资源。
第1期 刘传勇,等 G eosat/gM 7 Geosat/GM G eo sat/GM (%) (%) <502774517228746641193981582 <50277451722874681345050951 50~10026374163773994633928775017 50-100263741637739981575065233 1Q0~20043737271592603869124025858 1002004373727.1592601661810319240 200~3Q0286251777519884685258354 2003002862517.7751981636910164618 00-40163791017082821301.322661 400~50083285171418 7600471935 300~40063791017082815409587740 50~1000906156265875260326629 400~50083285171418141728800353 >I00 7900490564 60003726 50~1000906156265875431533727856 161039 161039 279.086972 >1000 790Q4905642783417284012 174673959 271.222701 108581286 161039 161039 8676582 0002709 279086972 282488836 ±26861316 ±11600294 271.222701 -260671770 8676582 2451268 4 T/P ±26861316 ±71.519863 G eosat/GM T/P T/P T/P T/P T/P Geosat/o T/P T/P Geosat/GM (%) <5081713740330452376067947 009051522031 415708099 Geosat/GM 1Q0~2001944326942483916575850 200~30014052362933 751.261352 36 300~4005779704002 160269088 400~5001742926337 60100908 Runge 500~10001181984527 10016818 >I000 60100908 00000000 5946 5946 26.86 ±11 53795687 l16709533 48781092 16002809 0018339 22162607 ±6055827 1994-2013ChinaAcademicJournalElectronicpUblishingHousealrightsreservedhttp://www.cnki.net 8 海洋测绘 第28卷 T/P Geosat/GM ±22.1626am ±6.0558m J 2006(6):37 39 2000 [M]. 2003. G eosat/GM 988 G eosat/M Runge [M] ,I982 [M] GEOSAT GM 1995 GEOSAT /GM T/P [M] The a pp lication of Posteriori C am pen sa tion Theory of error in A ltm eter d ata Set from G eo sat/GM Crossover a djusm ent LI Chuarryong', Bao Jng-y ang, HUANG Mo-tao, OUYANG Y ong-zhong LU X iu-png, li Chur-ju, ZHANG X in (lN aval Institu te of Hy dro graph ic Survey ing and C hartig Tian jin, 30006l; 2 D eparm ent of Hydrog raphy and C arbg raphy, D il an Naval A cadem y, Dalian L iaon ng 1 1601& 3 Navy Press T injin 300450 Abstract In order to e lim inate the inconsistency o f the ex isting da ta from m u lti- satellitem issing we use a new m e thod for he cro ssover ad justm ent w h ich is m od if ed to a t o step s pro cessing based on the a poste rori com pensation h eo ry of error The theory of to steps pro cessing used n G eo sat/GM crossover po in t adjusm ent Statistics o f crossover po int Ssh diffe ren ces be fo re and after crossover ad iu stm ent is anom a l, B ased on an analy sis of the orb it theory of g eo sat/Gm a ltm eter satellite the result show h isis r ungel phenom enon A m odif ed cam pute m odel for crossover ad jusm ent from altim eter da ta is pro po sed The new so li tin p o cedure is u scd b bo h local and global crossover ad j stm cnt p obkm. The com putatin rosu Its arc uscd to prove he ffic in cy and rc lab ility of the m od if icd m ethod Key wo rds sa te lite altim etry; cID ssover ad j sm ent Rungel phenom enon 1994-2013ChinaAcademicJournaleLectronicPublishingHouse.Allrightsreservedhttp://www.cnki.net

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