Abstract
This paper reports a series of comparisons of geoidal heights derived from several GOCE models with (1) geoidal heights derived from GPS on benchmarks (referred to as geometric geoidal heights) over Mexico and Canada, and with (2) geoidal heights derived from the latest geoidal maps of Mexico (GGM2010) and Canada (PCGG2013) (referred to as gravimetric geoidal heights). The paper also looks quantitatively into omission errors. Comparison (1) and (2) were carried out not including and including omission errors. The GOCE models used in comparison (1) disregarding omission errors are the direct solution model (first, second and third generations), the time-wise solution model (first, second and third generations), GOCO02S model and GIF48 model, all evaluated up to their maximum degree/order. Only GOCE direct third generation model was used in comparison (1) considering omission errors, and in comparison (2) disregarding omission errors, the latter with respect to GGM2010. The GOCE models used in comparison (2) including correction for omission errors are the GOCE direct third generation, GOCO01S, GOCO03S and DGM-1S models, evaluated up to degree/order 180. This makes GOCE direct third generation as the only model common in all comparisons. Omission errors were evaluated based on the extra-high degree harmonics of EGM2008. The omission errors in Mexico and in Canada show a similar behaviour, with a near zero mean and a standard deviation at the order of ±50 cm in Mexico and ±45 cm in Canada. In both cases, maximum differences reach more than 4 m. The effect of omission errors can be better appreciated by looking at performance of the only GOCE model used in all comparisons, the direct third generation model. Comparing it with Mexican geometric geoidal heights: without correcting for omission errors, mean and standard deviation of −5.1 and ±45.7 cm; including correction for omission errors, mean and standard deviation of −1.6 ± 30.6 cm. Comparing it with GGM2010: without correcting for omission errors, mean and standard deviation of −17.4 and ±51.3 cm; including correction for omission errors, mean and standard deviation of −2.8 ± 34.8 cm.
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ESA (1999) Gravity field and steady-state ocean circulation mission. Reports for Mission Selection, the Four Candidate Earth Explorer Core Missions, ESA SP-1233(1)
Featherstone W (2011) Absolute and relative testing of gravimetric geoid models using global positioning system and orthometric height data. Comput Geosci 27:807–814
Huang J, Véronneau M (2013) Canadian gravimetric geoid model 2010. J Geod. doi:10.1007/s00190-013-0645-0
ICGEM (2013) Global gravity models – table of models. [On-line] http://icgem.gfz-potsam.de/ICGEM/. Accessed Aug 2013
Muoz-Abundes R (2011) Geoide Gravimetrico Mexicano 2010 (GGM10). Technical Report of the Instituto Nacional de Estadistica y Geografia, Aguascalientes, Mexico
Pavlis N (1996) A modification to the program f477. Department of Geodetic Science and Surveying Technical Report, Ohio State University, Columbus, Ohio
Pavlis NK, Holmes SA, Kenyon SC, Factor JK (2012) The development and evaluation of the earth gravitational model 2008 (EGM2008). J Geophys Res 117(B4):2156–2202. doi:10.1029/2011JB008916
Pavlis NK, Holmes SA, Kenyon SC, J. K. Factor (2013) Correction to the development and evaluation of the earth gravitational model 2008 (EGM2008). J Geophys Res 118(5):2633. doi:10.1002/jgrb.50167
Peet T, Santos MC, Avalos D, Vaníček P, Huang J (2012) Assessment of GOCE models over Canada and Mexico. Book of Abstracts, 2012 CWRA-CGU National Conference, Banff, AB, 5–8 June, 31
Rapp RH (1982) A FORTRAN program for the computation of gravimetric quantities from high degree spherical harmonic expansions. Department of Geodetic Science and Surveying Technical Report No. 334, Ohio State University, Columbus, Ohio
Reigber CH, Schmidt R, Flechtner F, Konig R, Meyer U (2005) An earth gravity field model complete to degree and order 150 from GRACE: Eigen-Grace02S. J Geod 39:1–10
Rummel R (2012) Personal communication. TU Munich
Visser P, Rummel R, Balmino G, Sünkel H, Johannensen J, Aguirre M, Woodworth PL, le Provost C, Tsherning CC, Sabadini R (2002) The European earth explorer mission GOCE: impact for the geosciences. Ice Sheets, Sea Level and the Dynamic Earth, Geodynamics Series. Am Geophys Union 29:95–107. doi 10.1029/029GD06
Acknowledgements
Thanks to Natural Resources Canada and to Instituto Nacional de Estadística y Geografía for the provision of the geoid models PCGG2013 and GGM2010. GOCE models were obtained through ICGEM’s website, also cordially acknowledged.
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Santos, M.C., Avalos, D., Peet, T., Sheng, M., Kim, D., Huang, J. (2015). Assessment of GOCE Models Over Mexico and Canada and Impact of Omission Errors. In: Rizos, C., Willis, P. (eds) IAG 150 Years. International Association of Geodesy Symposia, vol 143. Springer, Cham. https://doi.org/10.1007/1345_2015_28
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DOI: https://doi.org/10.1007/1345_2015_28
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