 Express Letter
 Open access
 Published:
Evaluation of GOCEbased global gravity field models over Japan after the full mission using freeair gravity anomalies and geoid undulations
Earth, Planets and Space volume 69, Article number: 135 (2017)
Abstract
The performance of Gravity field and steadystate Ocean Circulation Explorer (GOCE) global gravity field models (GGMs), at the end of GOCE mission covering 42 months, is evaluated using geoid undulations and freeair gravity anomalies over Japan, including six subregions (Hokkaido, north Honshu, central Honshu, west Honshu, Shikoku and Kyushu). Seventeen GOCEbased GGMs are evaluated and compared with EGM2008. The evaluations are carried out at 150, 180, 210, 240 and 270 spherical harmonics degrees. Results show that EGM2008 performs better than GOCE and related GGMs in Japan and three subregions (Hokkaido, central Honshu and Kyushu). However, GOCE and related GGMs perform better than EGM2008 in north Honshu, west Honshu and Shikoku up to degree 240. This means that GOCE data can improve geoid model over half of Japan. The improvement is only evident between degrees 150 and 240 beyond which EGM2008 performs better than GOCE GGMs in all the six regions. In general, the latest GOCE GGMs (releases 4 and 5) perform better than the earlier GOCE GGMs (releases 1, 2 and 3), indicating the contribution of data collected by GOCE in the last months before the mission ended on 11 November 2013. The results indicate that a more accurate geoid model over Japan is achievable, based on a combination of GOCE, EGM2008 and terrestrial gravity data sets.
Background
The Gravity field and steadystate Ocean Circulation Explorer (GOCE) mission was launched on 17 March 2009 from the Plesetsk Cosmodrome in Russia by the European Space Agency (ESA). The GOCE mission finally ended on 11 November 2013. Several global gravity field models have been developed from GOCE data. The development of GOCEbased global gravity models has been achieved mainly by three strategies; direct solution (DIR), spacewise approach (SPW) and timewise solution (TIM). In addition, to the three ESA’s solutions mentioned, models based on a combination of GOCE data and other satellite only data sets have also been developed and are referred to as combined satellite field model (GOCO). GOCEbased GGMs developed until the end of the mission include: DIR (releases 1, 2, 3, 4, and 5), TIM (releases 1, 2, 3, 4 and 5), SPW (releases 1, 2 and 4) and GOCO (releases 1, 2, 3 and 5). It should be noted that SPW (releases 3 and 5) and GOCO (release 4) are missing because they were not processed, hence not included in the current study.
GOCEbased GGMs have been evaluated in different parts of the world by several authors (e.g. Gruber et al. 2011; Janák and Pitoňák 2011; Hirt et al. 2011; Guimarães et al. 2012; Odera and Fukuda 2013, Yi et al. 2013; Yi and Rummel 2014; AbdElmotaal 2015; Cheng and Ries 2015; Godah et al. 2015; Hirt et al. 2015; Huang and Véronneau 2015). The GOCE mission aimed at providing the geoid and gravity anomalies with an uncertainty of 1–2 cm and 1 mGal, respectively, both at a resolution of 100 km, corresponding to spherical harmonic degree and order 200 (e.g. Pail et al. 2011). Precise geoid modelling is the first important step towards establishment of a geoidbased height system. Although new techniques for gravimetric geoid determination have been advanced in the last two decades or slightly more, e.g. remove–compute–restore (Schwarz et al. 1990) and least square modification of Stokes’s formula (Sjöberg, 2003), much of the improvements in longwavelength geoid information required in these techniques have been due to the contribution of recent dedicated satellite gravity missions [e.g. Gravity Recovery and Climate Experiment (GRACE), Challenging Minisatellite Payload (CHAMP) and Gravity field and steadystate Ocean Circulation Explorer (GOCE)].
Odera and Fukuda (2013) investigated the contribution of the first released GOCEbased GGMs (DIR 1, 2, 3; TIM 1, 2, 3, SPW 1, 2 and GOCO 1, 2) in improvements of geoid model in the longwavelength components over Japan. The results showed that GOCEbased models could improve geoid model in Shikoku area only. In the current study, we carry out evaluation of GOCEbased models covering the entire GOCE mission using terrestrial freeair gravity anomalies and geometric geoid undulations over Japan. Further evaluations are carried out over each of the four main Japanese islands of Hokkaido, Honshu, Shikoku and Kyushu. Honshu Island is divided into three parts (north Honshu, central Honshu and west Honshu) due to its size and geometry.
Methods
Seventeen GOCEbased GGMs have been considered in the current evaluations (Table 1). Earth gravitational model of 2008 (EGM2008) is also included for comparative analysis. The assessment is based on geometric geoid undulations, obtained from 816 GPS/levelling points and freeair gravity anomalies, obtained from 6951 firstorder gravity points over Japan. The data were provided by the Geospatial Information Authority of Japan (http://www.gsi.go.jp/cais/spaceindexe.html). The approximate accuracy of GPS coordinates is ±1 cm horizontally and ±2 cm vertically. The maximum allowable accuracy of levelling data is approximated by \(15\sqrt K\) mm, where K is the levelling distance in km. The accuracy of gravity data is ±1 mGal. Figure 1 shows the distribution of GPS/levelling and firstorder gravity data over the four main islands of Japan. The number of GPS/levelling data points over the six subregions is: 163 for Hokkaido, 171 for north Honshu, 163 for central Honshu, 158 for west Honshu, 56 for Shikoku and 105 for Kyushu. The number of gravity data points over the six subregions are; 1431 for Hokkaido, 1368 for north Honshu, 1620 for central Honshu, 1166 for west Honshu, 401 for Shikoku and 965 for Kyushu. Although the Geospatial Information Authority of Japan has acquired a new set of GPS/levelling data at 971 points (Miyahara et al. 2014), including initially released 816 points used in this study, we do not expect significant differences in the common points. Also, such data sets were not available for the current research.
The evaluation of GOCEbased GGMs is carried out in two ways. The first method determines standard deviation of the differences between freeair gravity anomalies (obtained from observed gravity data in Japan) and freeair gravity anomalies implied by GOCEbased GGMs. The second method determines standard deviation of the differences between GPS/levelling geoid undulations (obtained from observed GPS and precise levelling data in Japan) and geoid undulations implied by GOCEbased GGMs. The freeair gravity anomalies and geoid undulations implied by GOCEbased GGMs are computed at intervals of degree 30 starting from 150 up to 270 spherical harmonic degrees. This is because all the GGMs considered perform practically at the same level for the wavelengths longer than degree 150.
The geoid undulation and freeair gravity anomaly implied by a GGM are generally obtained by Eqs. 1 and 2, respectively.
where N _{ o } and \(\Delta g_{o}\) are zeroorder degree terms for geoid undulation and gravity anomaly, respectively, C _{ T } is a conversion term used to convert height anomaly to geoid undulation, GM is the product of the universal gravitational constant and mass of the Earth, \(a_{\text{ref}}\) is a scaling parameter associated with a particular GGM, \(\bar{P}_{nm} (\cos \theta )\) are fully normalised associated Legendre functions for degree n and order m, \(\bar{C}_{nm}^{*}\) and \(\bar{S}_{nm}\) are fully normalised spherical harmonic coefficients after reduction by the even zonal harmonics of the reference ellipsoid, and n _{max} is the finite maximum degree of a GGM.
Results
The statistics of the differences between observed and GOCEbased GGMs implied gravity anomalies in Japan, and the six subregions are presented in Fig. 2. Consequently, the statistics of the differences between observed and GOCEbased GGMs implied geoid undulations in Japan and the six subregions are presented in Fig. 3. Corresponding results for EGM2008 are also included for comparative analysis. The models are truncated at 150, 180, 210, 240 and 270 spherical harmonic degrees, where the maximum degrees for each model allow.
It is observed that the performance of GOCEbased GGMs over Japan is practically the same at degree 150 for both freeair gravity anomalies (Fig. 2) and geoid undulations (Fig. 3). They also perform at the same level with EGM2008, although some GOCEbased GGMs perform slightly better than EGM2008 at degree 150 for geoid undulations (SPW1, 2, DIR1, TIM2) and gravity anomalies (GOCO1, 2, 3). The latest GOCE GGMs (releases 4 and 5) do not improve the performance over the earlier released GGMs (releases 1, 2, 3) in Japan at degree 150. Similar patterns are noted over the six subregions of Hokkaido, north Honshu, central Honshu, west Honshu, Shikoku and Kyushu.
There is a slight difference in the performance of GOCEbased GGMs over Japan (only 0.2 mGal and 0.8 cm for gravity anomalies and geoid undulations, respectively) at 180 spherical harmonic degrees. EGM2008 performs slightly better than GOCEbased GGMs over Japan at degree 180. However, gravity anomalies comparisons show that SPW4 and DIR4 perform at the same level with EGM2008 in Kyushu, while GOCO2, TIM2 and DIR2 interestingly perform better than EGM2008 in west Honshu and most GOCEbased GGMs perform better than EGM2008 in Shikoku at degree 180. On the other hand, geoid undulations comparisons show that GOCO5 and DIR5 perform slightly better than EGM2008 in north Honshu, while most GOCEbased GGMs perform better than EGM2008 in west Honshu and all GOCEbased GGMs perform better than EGM2008 in Shikoku at degree 180. Generally, the latest GOCEbased GGMs (releases 4 and 5) improve the performance over the first GGMs (releases 1, 2 and 3) at 180 and higher degrees over Japan. Although some surprises are also noted where early releases of GOCEbased GGMs perform better than the latest releases, such surprises are extremely minimal with timewise solution (TIM). This indicates a good consistency in the GOCE data. It also indicates that more data collected by GOCE in the last months of operation have improved the performance of GOCEbased GGMs in the longtomedium wavelength components.
Comparisons at degrees 210–270 show that EGM2008 performs better than GOCEbased GGMs over Japan. Although gravity anomalies show that some GOCEbased GGMs perform slightly better than EGM2008 between degrees 210 and 240 in north Honshu, central Honshu, west Honshu, Shikoku and Kyushu, independent check by geoid undulations show that GOCE GGMs perform better than EGM2008 only in Shikoku (at degree 210, best models are DIR5, TIM5 and GOCO5 and at degree 240, best models are DIR4 and SPW4) and west Honshu (at degree 210, best models are TIM5, TIM4 and GOCO5). The best models referred to here perform practically at the same level. EGM2008 performs better than GOCEbased GGMs over Japan and all the six subregions at 270 spherical harmonic degrees. TIM5 performs better than other GOCEbased GGMs over Japan at degree 270 when both geoid undulations and gravity anomalies are considered.
At the end of GOCE mission, GOCEbased GGMs now perform better than EGM2008 in north Honshu (up to degree 180), west Honshu (up to degree 210) and Shikoku (up to degree 240). GOCEbased GGMs can now significantly improve geoid model in Japan if combined with EGM2008 to cater for the omission errors in the mediumtoshort wavelength components over the three subregions in Japan. This is approximately half of the area of study in terms of spatial extents. There is no significant evidence of geoid model improvement by GOCEbased GGMs over EGM2008 in Hokkaido, Central Honshu and Kyushu regions. It is noted that all GGMs evaluated perform poorly in the mountainous area of central Honshu, for gravity anomalies (Fig. 2c) beyond degree 180. This indicates a general decline in the accuracy of GGMs in the mediumtoshort wavelength components in mountainous areas. However, the trend is not replicated in the geoid undulation differences (Fig. 3c) because most GPS/levelling data have low elevations (<1000 m) even in mountainous areas like central Honshu (e.g. Odera and Fukuda 2015). It is also noted that GOCE GGMs perform relatively better in Kyushu (considering the magnitude of standard deviation) than other regions over Japan (Figs. 2f, 3f). This may be attributed to the fact that Kyushu Island is in a relatively lower elevation terrain than the other regions considered in the current study.
Conclusions
This study represents a comprehensive assessment of GOCE data and possible contribution of GOCE GGMs in geoid modelling over Japan covering the entire GOCE mission. Seventeen GOCEbased GGMs (releases 1, 2, 3, 4 and 5) have been evaluated over Japan using gravity anomalies (from firstorder gravity data) and geoid undulations (from GPS/levelling data) at 150, 180, 210, 240 and 270 spherical harmonic degrees. A general consistency in GOCE data is observed in the increasing accuracy with increase in length of observations. The latest GGMs (releases 4 and 5) perform better than the earlier released GGMs (releases 1, 2 and 3) but only after 150 spherical harmonic degrees. All the GOCEbased GGMs evaluated and EGM2008 perform practically at the same level at degree 150 over Japan. Improvement of geoid model over Japan by GOCE GGMs is evident in north Honshu (up to degree 180), west Honshu (up to degree 210) and Shikoku (up to degree 240), with significant improvement at degree 180. EGM2008 performs better than GOCEbased GGMs in Hokkaido, Central Honshu and Kyushu over the same range of spherical harmonic degrees. Following possibilities of further improvement of the geoid model over approximately half of Japan by GOCE data, we intend to develop a more improved geoid model for Japan based on GOCE data (in north Honshu, west Honshu and Shikoku), EGM2008 and terrestrial gravity data using the method described in Odera and Fukuda (2014).
Abbreviations
 CHAMP:

Challenging Minisatellite Payload
 DIR:

direct solution
 EGM2008:

earth gravitational model of 2008
 ESA:

European Space Agency
 GGM:

global gravity model
 GOCE:

Gravity field and steadystate Ocean Circulation Explorer
 GOCO:

combined satellite field model
 GPS:

Global Positioning System
 GRACE:

Gravity Recovery and Climate Experiment
 LAGEOS:

Laser Geodynamics Satellite
 SLR:

satellite laser ranging
 SPW:

spacewise approach
 TIM:

timewise solution
References
AbdElmotaal HA (2015) Validation of GOCE models in Africa. Newton’s Bull 5:149–162
Brockmann JM, Zehentner N, Höck E, Pail R, Loth I, MayerGürr T, Schuh WD (2014) EGM_ TIM_RL05: an independent geoid with centimeter accuracy purely based on the GOCE mission. Geophys Res Lett 41(22):8089–8099
Bruinsma SL, Marty JC, Balmino G, Biancale R, Förste C, Abrikosov O, Neumayer H (2010) GOCE gravity field recovery by means of the direct numerical method. Presented at the ESA living planet symposium, June 27–July 2, 2010, Bergen, Norway
Bruinsma SL, Förste C, Abrikosov O, Marty JC, Rio MH, Mulet S, Bonvalot S (2013) The new ESA satelliteonly gravity field model via the direct approach. Geophys Res Lett 40(14):3607–3612
Cheng M, Ries JC (2015) Evaluation of GOCE gravity models with SLR orbit tests. Newton’s Bull 5:187–192
Gatti A, Reguzzoni M, Migliaccio F, Sansò F (2014) Spacewise grids of gravity gradients from GOCE data at nominal satellite altitude. Presented at the 5th international GOCE user workshop, November 25–28, 2014, Paris, France
Godah W, Krynski J, Szelachowska M (2015) On the accuracy assessment of the consecutive releases of GOCEbased GGMs over the area of Poland, Assessment of GOCE Geopotential Models. Newton’s Bull 5:49–62
Goiginger H, Höck E, Rieser D, MayerGürr T, Maier A, Krauss S, Pail R, Fecher T, Gruber T, Brockmann JM, Krasbutter I, Schuh WD, Jäggi A, Prange L, Hausleitner W, Baur O, Kusche J (2011) The combined satelliteonly global gravity field model GOCO02S. Presented at the 2011 general assembly of the European geosciences union, April 4–8, 2011, Vienna, Austria
Gruber T, Visser PNAM, Ackermann Ch, Hosse M (2011) Validation of GOCE gravity field models by means of orbit residuals and geoid comparisons. J Geodesy 85:845–860
Guimarães G, Matos A, Blitzkow D (2012) An evaluation of recent GOCE geopotential models in Brazil. J Geod Sci 2(2):144–155
Hirt C, Gruber T, Featherstone WE (2011) Evaluation of the first GOCE static gravity field models using terrestrial gravity, vertical deflections and EGM2008 quasigeoid heights. J Geodesy 85:723–740
Hirt C, Rexer M, Claessens S (2015) Topographic evaluation of fifthgeneration GOCE gravity field models globally and regionally. Newton’s Bull 5:163–186
Huang J, Véronneau M (2015) Assessments of recent GRACE and GOCE release 5 global geopotential models in Canada. Newton’s Bull 5:127–148
Janák J, Pitoňák M (2011) Comparison and testing of GOCE global gravity models in Central Europe. J Geod Sci 1:333–347
MayerGürr T, Rieser D, Höck E, Brockmann JM, Schuh WD, Krasbutter I, Kusche J, Maier A, Krauss S, Hausleitner W, Baur O, Jäggi A, Meyer U, Prange L, Pail R, Fecher T, Gruber T (2012) The new combined satellite only model GOCO03s. Presented at the international symposium on gravity, geoid and height systems GGHS 2012, International Association of Geodesy, October 9–12, 2012, Venice, Italy
MayerGürr T, Pail R, Gruber T, Fecher T, Rexer M, Schuh WD, Kusche J, Brockmann JM, Rieser D, Zehentner N, Kvas A, Klinger B, Baur O, Höck E, Krauss S, Jäggi A (2015) The combined satellite gravity field model GOCO05s. Presentation at the EGU 2015, April 12–17, 2015, Vienna, Austria
Migliaccio F, Reguzzoni M, Sansò F, Tscherning CC, Veicherts M (2010) GOCE data analysis: the spacewise approach and the first spacewise gravity field model. Presented at the ESA living planet symposium, June 27July 2, 2010, Bergen, Norway
Migliaccio F, Reguzzoni M, Gatti A, Sansò F, Herceg M (2011) A GOCEonly global gravity field model by the spacewise approach. Presented at the 4th international GOCE user workshop, March 31April 1, 2011, Munich, Germany
Miyahara B, Kodama T, Kuroishi Y (2014) Development of new hybrid geoid model for Japan, “GSIGEO2011”. Bull Geospat Inf Auth Jpn 62:11–20
Odera PA, Fukuda Y (2013) Towards an improvement of the geoid model in Japan by GOCE data: a case study of the Shikoku area. Earth Planets Space 65(4):361–366. doi:10.5047/eps.2012.07.005
Odera PA, Fukuda Y (2014) Improvement of the geoid model over Japan using integral formulae and combination of GGMs. Earth Planets Space 66:22. doi:10.1186/188059816622
Odera PA, Fukuda Y (2015) Comparison of Helmert and rigorous orthometric heights over Japan. Earth Planets Space 67:27. doi:10.1186/s4062301501942
Pail R, Goiginger H, Mayrhofer R, Schuh WD, Brockmann JM, Krasbutter I, Höck E, Fecher T (2010a) GOCE gravity field model derived from orbit and gradiometry data applying the timewise method. Presented at the ESA living planet symposium, June 27–July 2, 2010, Bergen, Norway
Pail R, Goiginger H, Schuh WD, Höck E, Brockmann JM, Fecher T, Gruber T, MayerGürr T, Kusche J, Jäggi A, Rieser D (2010b) Combined satellite gravity field model GOCO01S derived from GOCE and GRACE. Geophys Res Lett. doi:10.1029/2010GL044906
Pail R, Bruinsma S, Migliaccio F, Forste CF, Goiginger H, Schuh WD, Höck E, Reguzzoni M, Brockmann JM, Abrikosov O, Veicherts M, Fecher T, Mayrhofer R, Krasbutter I, Sansò F, Tscherning CC (2011) First GOCE gravity field models derived by three different approaches. J Geod 85:819–843
Pavlis NK, Holmes SA, Kenyon SC, Factor JK (2012) The development and evaluation of the Earth Gravitational Model (EGM2008). J Geophys Res. doi:10.1029/2011JB008916
Schwarz KP, Sideris M, Forsberg R (1990) The use of FFT techniques in physical geodesy. Geophys J Int 100:485–514
Sjöberg LE (2003) A computational scheme to model the geoid by the modified Stokes’s formula without gravity reductions. J Geodesy 77:423–432
Yi W, Rummel R (2014) A comparison of GOCE gravitational models with EGM2008. J Geodyn 73:14–22
Yi W, Rummel R, Gruber T (2013) Gravity field contribution analysis of GOCE gravitational gradient components. Stud Geophys Geod 57(2):174–202
Authors’ contributions
PAO and YF designed the research, and YF facilitated the data acquisition and interpretation. PAO carried out the computations and related analyses. He also wrote and revised the paper. Both authors read and approved the final manuscript.
Acknowledgements
We would like to thank the Geospatial Information Authority of Japan for providing GPS/levelling and gravity data sets covering the study area. Part of this research was conducted when the first author was a visiting scholar at Kyoto University, Geodesy Laboratory. We are grateful for the support granted to us by the Japan Student Services Organization through followup research fellowship programme. We appreciate the two anonymous reviewers, for their constructive comments and suggestions that have been used to improve the quality of the paper.
Competing interests
The authors declare that they have no competing interests.
Availability of data and materials
The GPS/levelling and gravity data used in this study can be obtained from the Geospatial Information Authority of Japan. The GGMs in form of spherical coefficients are freely available at the International Centre for Global Gravity Field Models website (http://icgem.gfzpotsdam.de/ICGEM/).
Consent for publication
Not applicable.
Ethics approval and consent to participate
Not applicable.
Publisher’s Note
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
Open Access This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.
About this article
Cite this article
Odera, P.A., Fukuda, Y. Evaluation of GOCEbased global gravity field models over Japan after the full mission using freeair gravity anomalies and geoid undulations. Earth Planets Space 69, 135 (2017). https://doi.org/10.1186/s4062301707161
Received:
Accepted:
Published:
DOI: https://doi.org/10.1186/s4062301707161