7. THE GRAVITY ANOMALIES DERIVED FROM GEOID HEIGHT DATA IN VIETNAM

Hoa Pham Thi, Thu Trinh Hoai

Giới thiệu

Both gravity anomaly and geoid height are features of the disturbing potential. Geoid undulations have been determined by gravity anomalies based on the solution of boundary value problem in the potential theory for a long time. Recently, with the broad application of the satellite altimeter data, geoid heights have been determined directly in large regions without gravity anomaly data. With the availability of geoid height data, the opposite direction of calculating gravity anomalies has been considered. This study aims to generate gravity anomaly data in Vietnam based on the least squares collocation approach, of which the correlation between gravity anomalies and geoid heights is the key point. At the same time, in order to simplify the calculation, remove - restore technique was applied. The results not only contributed to making the theory and process more defined, but also verified the determination of gravity anomaly data employing geoid undulations in Vietnam. Additionally, the results are of great significance in constructing a marine gravity model to study sea level rise, and provide information for further exploration and exploitation of marine resources.

Toàn văn bài báo

Được tạo từ tệp XML

Trích dẫn

[1]. Ahmed Abdo Ali, Liu Jing Nan and Jiang Wei Peng (2007). Determination of Gravity Anomalies over the Arabian Sea. Journal of Applied Sciences 7(6): 877-882
[2]. Bernhard Hofmann - Helmurt Moritz (2005). Physical Geodesy. Springer Wien NewYork.
[3]. Lemoine F. G et al (1998). EGM 96. The NASA GSFC and NIMA Joint Geopotential Model.
[4]. Neiman. Y. M. (2010). Covariance in Physical Geodedy and Collocation. Moscow.
[5]. Pham Hoang Lan (1972). Gravity for Geodesy book. Hanoi University of Mining and Geology, Hanoi (Vietnames eddition)
[6]. Rene Forsberg (2003). An overview manual for the GRAVSOFT Geodetic Gravity Field Modelling Programs
[7]. Sandwell DT, Smith WHF (1997). Marine gravity anomaly from Geosat and ERS 1 satellite altimetry. J Geophys Res 102:10 039-10 054.
[8]. Seeber, Gunter (2003). Satellite geodesy. 2nd edition. Walter de Gruyte, Berlin New York.
[9]. Tscherning C., Forsberg R,. Knudsen P (1992). The GRAVSOFT package for geoid determination. First Continental Workshop On The Geoid In Europe “Towards a Precise Pan-European Reference Geoid for the Nineties” Prague, May 11 - 14.
[10]. https://www.aviso.altimetry.fr/en/techniques/altimetry.html.

Các tác giả

Hoa Pham Thi
phamhoa9.9.1978@gmail.com (Liên hệ chính)
Thu Trinh Hoai
Pham Thi, H., & Trinh Hoai, T. (2019). 7. THE GRAVITY ANOMALIES DERIVED FROM GEOID HEIGHT DATA IN VIETNAM. Tạp Chí Khoa học Tài Nguyên Và Môi trường, (21), 57–65. Truy vấn từ http://tapchikhtnmt.hunre.edu.vn/index.php/tapchikhtnmt/article/view/102
##submission.license.notAvailable##

Chi tiết bài viết

Các bài báo tương tự

1 2 3 4 5 > >> 

Bạn cũng có thể bắt đầu một tìm kiếm tương tự nâng cao cho bài báo này.