DETERMINISTICALLY-MODIFIED INTEGRAL ESTIMATORS OF GRAVITATIONAL TENSOR
The Earth's global gravity field modelling is an important subject in Physical Geodesy. For this purpose different satellite gravimetry missions have been designed and launched. Satellite gravity gradiometry (SGG) is a technique to measure the second-order derivatives of the gravity field. The...
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Online Access: | https://doi.org/10.1590/S1982-217020150001000012 https://doaj.org/article/2937f8b4717c481b93347ba9ec4ac210 |
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fttriple:oai:gotriple.eu:oai:doaj.org/article:2937f8b4717c481b93347ba9ec4ac210 2023-05-15T16:11:56+02:00 DETERMINISTICALLY-MODIFIED INTEGRAL ESTIMATORS OF GRAVITATIONAL TENSOR DETERMINISTICALLY-modified INTEGRAL Estimators OF GRAVITATIONAL TENSOR Mohsen Romeshkani Mehdi Eshagh https://doi.org/10.1590/S1982-217020150001000012 https://doaj.org/article/2937f8b4717c481b93347ba9ec4ac210 pt por Universidade Federal do Paraná 1982-2170 doi:10.1590/S1982-217020150001000012 https://doaj.org/article/2937f8b4717c481b93347ba9ec4ac210 undefined Boletim de Ciências Geodésicas, Vol 21, Iss 1, Pp 189-212 : Isotropic Kernels Gravity Anomalies Gravity Gradients Modification Simulation of Gravitational Tensor Truncation Coefficients geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ fttriple https://doi.org/10.1590/S1982-217020150001000012 2023-01-22T18:29:24Z The Earth's global gravity field modelling is an important subject in Physical Geodesy. For this purpose different satellite gravimetry missions have been designed and launched. Satellite gravity gradiometry (SGG) is a technique to measure the second-order derivatives of the gravity field. The gravity field and steady state ocean circulation explorer (GOCE) is the first satellite mission which uses this technique and is dedicated to recover Earth's gravity models (EGMs) up to medium wavelengths. The existing terrestrial gravimetric data and EGM scan be used for validation of the GOCE data prior to their use. In this research, the tensor of gravitation in the local north-oriented frame is generated using deterministically-modified integral estimators involving terrestrial data and EGMs. The paper presents that the SGG data is assessable with an accuracy of 1-2 mE in Fennoscandia using a modified integral estimatorby the Molodensky method. A degree of modification of 100 and an integration cap size of for integrating terrestrial data are proper parameters for the estimator. Article in Journal/Newspaper Fennoscandia Unknown Boletim de Ciências Geodésicas 21 1 189 212 |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
fttriple |
language |
Portuguese |
topic |
: Isotropic Kernels Gravity Anomalies Gravity Gradients Modification Simulation of Gravitational Tensor Truncation Coefficients geo |
spellingShingle |
: Isotropic Kernels Gravity Anomalies Gravity Gradients Modification Simulation of Gravitational Tensor Truncation Coefficients geo Mohsen Romeshkani Mehdi Eshagh DETERMINISTICALLY-MODIFIED INTEGRAL ESTIMATORS OF GRAVITATIONAL TENSOR |
topic_facet |
: Isotropic Kernels Gravity Anomalies Gravity Gradients Modification Simulation of Gravitational Tensor Truncation Coefficients geo |
description |
The Earth's global gravity field modelling is an important subject in Physical Geodesy. For this purpose different satellite gravimetry missions have been designed and launched. Satellite gravity gradiometry (SGG) is a technique to measure the second-order derivatives of the gravity field. The gravity field and steady state ocean circulation explorer (GOCE) is the first satellite mission which uses this technique and is dedicated to recover Earth's gravity models (EGMs) up to medium wavelengths. The existing terrestrial gravimetric data and EGM scan be used for validation of the GOCE data prior to their use. In this research, the tensor of gravitation in the local north-oriented frame is generated using deterministically-modified integral estimators involving terrestrial data and EGMs. The paper presents that the SGG data is assessable with an accuracy of 1-2 mE in Fennoscandia using a modified integral estimatorby the Molodensky method. A degree of modification of 100 and an integration cap size of for integrating terrestrial data are proper parameters for the estimator. |
format |
Article in Journal/Newspaper |
author |
Mohsen Romeshkani Mehdi Eshagh |
author_facet |
Mohsen Romeshkani Mehdi Eshagh |
author_sort |
Mohsen Romeshkani |
title |
DETERMINISTICALLY-MODIFIED INTEGRAL ESTIMATORS OF GRAVITATIONAL TENSOR |
title_short |
DETERMINISTICALLY-MODIFIED INTEGRAL ESTIMATORS OF GRAVITATIONAL TENSOR |
title_full |
DETERMINISTICALLY-MODIFIED INTEGRAL ESTIMATORS OF GRAVITATIONAL TENSOR |
title_fullStr |
DETERMINISTICALLY-MODIFIED INTEGRAL ESTIMATORS OF GRAVITATIONAL TENSOR |
title_full_unstemmed |
DETERMINISTICALLY-MODIFIED INTEGRAL ESTIMATORS OF GRAVITATIONAL TENSOR |
title_sort |
deterministically-modified integral estimators of gravitational tensor |
publisher |
Universidade Federal do Paraná |
url |
https://doi.org/10.1590/S1982-217020150001000012 https://doaj.org/article/2937f8b4717c481b93347ba9ec4ac210 |
genre |
Fennoscandia |
genre_facet |
Fennoscandia |
op_source |
Boletim de Ciências Geodésicas, Vol 21, Iss 1, Pp 189-212 |
op_relation |
1982-2170 doi:10.1590/S1982-217020150001000012 https://doaj.org/article/2937f8b4717c481b93347ba9ec4ac210 |
op_rights |
undefined |
op_doi |
https://doi.org/10.1590/S1982-217020150001000012 |
container_title |
Boletim de Ciências Geodésicas |
container_volume |
21 |
container_issue |
1 |
container_start_page |
189 |
op_container_end_page |
212 |
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1765997148814442496 |