Heterogeneous data management and modeling for the gravimetric geoid model: a review study in Pakistan
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  • 作者:Muhammad Sadiq ; Zulfiqar Ahmad
  • 关键词:Gravimetric geoid model ; Digital elevation model ; Standard deviation
  • 刊名:Arabian Journal of Geosciences
  • 出版年:2015
  • 出版时间:April 2015
  • 年:2015
  • 卷:8
  • 期:4
  • 页码:2247-2263
  • 全文大小:6,566 KB
  • 参考文献:1. BGP (2000). Premier oil company gravity survey of Kalat, Pakistan, BGP crew 9501G final reports (internal), Bureau of Geophysical Prospecting (Pakistan) International, November, 2000
    2. Farr, TG, Kobrick, M (2000) Shuttle radar topography mission produces a wealth of data. Am Geophys Union Eos 81: pp. 583-585 CrossRef
    3. Featherstone W. E. (2002) “Report of IAG Special Study Group 3.177 Synthetic Modelling of the Earth’s Gravity Field (1999-001),-Report of the IAG 3.177, Preprint from http://www.cage.curtin.edu.au/will/iags sg3 177.html. Millennium. Springer, Berlin Heidelberg New York, pp 163-71
    4. Forsberg, R (1984) Local covariance functions and density distributions. Report no.356. Dept. of Geodetic Science, Ohio State University, Columbus, Ohio
    5. Forsberg, R, Tscherning, CC (1981) The use of height data in the gravity field approximation by collocation. September 10, 1981. JGR 86: pp. 7843-7854 CrossRef
    6. GETECH (1995) GETECH report on South East Asia Gravity project (SEAGP), GETECH Group plc., Kitson House, Elmete Hall Elmete Lane, Roundhay University of Leeds, LS8 2LJ, UK
    7. GRAVSOT (2005) A System for Geodetic Gravity Field Modelling. C.C. Tscherning, Department of Geophysics, Juliane Maries Vej 30, DK-2100 Copenhagen N. R. Forsberg and P. Knudsen, Kort og Matrikelstyrelsen, Rentemestervej-8, DK-2400 Copenhagen NV
    8. Hastings, DA, Dunbar, PK (1999) Global land one-kilometer base elevation (GLOBE): NGDC key to geophysical records documentation No. 34. National Geophysical Data Center, Boulder Colorado
    9. Helmut, L (1965) A generalized form of Nettletons’s density determination. Geophys Prospect 15: pp. 247-258
    10. Hunegnaw, A (2001) The effect of lateral density variation on local geoid determination, Proc. IAG 2001. Scientific Assembly, Budapest, Hungary
    11. Kiamehr, R (2006) The impact of lateral density variation model in the determination of precise gravimetric geoid in mountainous areas: a case study of Iran. Geophys J Int 167: pp. 521-527 CrossRef
    12. Kirby JF, Featherstone WE, Kearsley AHW (1998) Tests of the DMA/GSFC geopotential models over Australia. Geophys J Int 7:2-3
    13. Kuhtreiber, N (1998) Precise geoid determination using a density variation model. Phys Chem Earth 23: pp. 59-63(5) CrossRef
    14. Lemoine FG, Smith DE, Smith R, Kunz L, Pavlis NK, Klosko SM, Chinn DS, Torrence MH, Williamson RG, Cox CM, Rachlin KE, Wang YM, Pavlis EC, Kenyon SC, Salman R, Trimmer R, Rapp RH, Nerem RS (1997) The development of the NASA, GSFC and NIMA joint geopotential model. In: Segawa, Fugimoto and Okubo (eds) IAG Synzposza 117: Gravzly, Geozd, and Marzne Geodesy, Springer-Verlag, Berlin, pp. 461-70
    15. Lemoine FG, Kenyon SC, Factor JK, Trimmer RG, Pavlis NK, Chinn DS, Cox CM, Klosko SM, Luthcke SB, Torrence MH, Wang YM, Williamson RG, Pavlis EC, Rapp RH, Olson TR (1998). The development of the joint NASA GSFC and the National Imagery and Mapping Agency (NIMA) geopotential model EGM96, NASA/TP- 1998-06861, Goddard Space Flight Center, National Aeronautics and Space Administration, Greenbelt
    16. Martinec, Z (1993) Effect of lateral density variations of topographical masses in view of improving geoid model accuracy over Canada. Contract report for Geodetic Survey of Canada, Ottawa, Canada
    17. Molodensky, MS, Eremeev, VF, Yurkina, MI (1962) Methods for the study of the external gravitational field and figure of the Earth. Israeli Program for Scientific Translations, Jerusalem
    18. Nahavandchi, H (2002) Two different methods of geoidal height determinations using a spherical harmonics representation of the geopotential topographic corrections and height anomaly-geoidal height difference. J Geod 76: pp. 345-352 CrossRef
    19. Nettleton LL (1971) Elementary gravity and magnetic for geologists and seismologists. SEG Books, Technology & Engineering, p 121
    20. Noor E, Chen J, Yulin L, Zhang J (1997) Report on data processing/adjustment regarding “A-& “AB-order GPS networks of Pakistan, Survey of Pakistan Rawalpindi
    21. Pavlis NK, Chinn DS, Cox CM, Lemoine FG (2000) Geopotential model improvement using POCM_4B dynamic ocean topography information: PGM2000A, paper presented at the Joint TOPEX/Poseidon and Jason-1
  • 刊物类别:Earth and Environmental Science
  • 出版者:Springer Berlin Heidelberg
  • ISSN:1866-7538
文摘
The gravimetric geoid model can be used as vertical reference in surveying and other related technologies. It is being developed by NESCOM in collaboration with the Department of Earth sciences QAU, Survey of Pakistan and Directorate General of Petroleum Concessions (DGPC). The data collection, selection, and analysis to make the data suitable for this purpose are being carried out. About 77,834 land gravity observations along with leveling and 11,787 Bouguer/free-air anomalies from GTECH are available and readily accessible. While GPS/leveling data for the whole Pakistan region is required and is being collected from different sources, though its density and quantity is not good enough for better calibration of gravimetric geoid. This study involves the feasibility and application of different datasets for the development of geoid model of Pakistan. The SRTM30 digital elevation model has been selected for topographic corrections and reductions due to its relatively better statistical comparison with local elevation data. Both least square collocation and FFT methods have been applied for this study. Two realistic studies have been carried out for global geopotential model selection based on statistical findings and evaluation of geoid-quasigeoid separation term in Pakistan. Geoid-quasigeoid separation term is an integral part of “Restore step-for geoid modeling with the utilization of the solution of the Molodensiky’s geodetic boundary value problem. The digital elevation model comparison with local leveling data shows that SRMT30 model is relatively better in accuracy (in terms of mean and standard deviation) than other counterparts such as Globe30, GTOPO30, and ETOPO2, etc. The results of geoid modeling have revealed that there exists a height bias of ?0?cm between local vertical datum and global mean sea level.

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