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فیزیک زمین و فضا، جلد ۴۰، شماره ۳، صفحات ۳۵-۴۶
عنوان فارسی Gravity acceleration at the sea surface derived from satellite altimetry data using harmonic splines
چکیده فارسی مقاله Gravity acceleration data have grand pursuit for marine applications. Due to environmental effects, marine gravity observations always hold a high noise level. In this paper, we propose an approach to produce marine gravity data using satellite altimetry, high-resolution geopotential models and harmonic splines. On the one hand, harmonic spline functions have great capability for local gravity field modeling. On the other hand, the information from satellite altimetry is a viable source of information for the marine gravimetry in the high-frequency gravity field modeling. Marine geoid from satellite altimetry observations can be converted to disturbing potential via ellipsoidal Bruns’s formula. The reference gravity field’s contribution is removed and restored after solving Dirichlet Boundary Value Problem. Finally, the results are downward continued to the sea surface using free air scheme. Computation of gravity acceleration in the Persian Gulf and its compatibility with the shipborne data shows reasonable performance of this methodology.
کلیدواژه‌های فارسی مقاله Harmonic splines، Shipborne gravimetry، Satellite altimetry، Gravity field modeling،
عنوان انگلیسی Gravity acceleration at the sea surface derived from satellite altimetry data using harmonic splines
چکیده انگلیسی مقاله Gravity acceleration data have grand pursuit for marine applications. Due to environmental effects, marine gravity observations always hold a high noise level. In this paper, we propose an approach to produce marine gravity data using satellite altimetry, high-resolution geopotential models and harmonic splines. On the one hand, harmonic spline functions have great capability for local gravity field modeling. On the other hand, the information from satellite altimetry is a viable source of information for the marine gravimetry in the high-frequency gravity field modeling. Marine geoid from satellite altimetry observations can be converted to disturbing potential via ellipsoidal Bruns’s formula. The reference gravity field’s contribution is removed and restored after solving Dirichlet Boundary Value Problem. Finally, the results are downward continued to the sea surface using free air scheme. Computation of gravity acceleration in the Persian Gulf and its compatibility with the shipborne data shows reasonable performance of this methodology.
کلیدواژه‌های انگلیسی مقاله Harmonic splines, Shipborne gravimetry, Satellite altimetry, Gravity field modeling
نویسندگان مقاله a صفری |
department of surveying and geomatics engineering, university college of engineering, university of tehran, tehran, iran
سازمان اصلی تایید شده: دانشگاه تهران (Tehran university)

محمدعلی شریفی | m a
department of surveying and geomatics engineering, university college of engineering, university of tehran, tehran, iran
سازمان اصلی تایید شده: دانشگاه تهران (Tehran university)

h امین |
department of surveying and geomatics engineering, university college of engineering, university of tehran, tehran, iran
سازمان اصلی تایید شده: دانشگاه تهران (Tehran university)

i فروغی |
department of surveying and geomatics engineering, university college of engineering, university of tehran, tehran, iran
سازمان اصلی تایید شده: دانشگاه تهران (Tehran university)

نشانی اینترنتی https://jesphys.ut.ac.ir/article_51597_48ab4d32c6bb6898d08bffa331bb8091.pdf
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