Spaceborne gravimetry and gravity field recovery

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Autoren

Organisationseinheiten

Externe Organisationen

  • University of Calgary
  • Universität Stuttgart
Forschungs-netzwerk anzeigen

Details

OriginalspracheEnglisch
Seiten (von - bis)65-75
Seitenumfang11
FachzeitschriftCanadian Aeronautics and Space Journal
Jahrgang53
Ausgabenummer3-4
PublikationsstatusVeröffentlicht - 2007

Abstract

As an integrated signal of mass transition and distribution, the Earth's gravity senses the inner and outer mass balance of the Earth. However, gravity cannot be measured directly in space but can be derived from other measurements obtained by space vehicles. The dedicated gravity field satellite missions CHAMP, GRACE, and GOCE serve as spaceborne gravimeters by utilizing satellite-to-satellite tracking (SST) and satellite gravity gradiometry (SGG) techniques. In this "decade of the geopotentials", these missions will serve different purposes with particular spatial and spectral resolutions. This paper introduces the usefulness of these missions, their impacts on the geosciences, the measurement principles, and their implementations. These space sensors will provide a significant number of observations during their mission lifespans. Therefore, global gravity field recovery is a computationally demanding task. Several approaches aimed at this goal are discussed, namely the brute-force approach, the space-wise approach, the time-wise approach, and the proposed torus-based semi-analytical approach. The paper addresses the characteristics of each approach and focuses mainly on the torus-based semi-analytical approach, which can be used to derive the gravity field from, any geopotential functional. In this approach, the structure of the normal matrix becomes block-diagonal, which leads to a powerful and efficient recovery tool through the use of the fast Fourier transform (FFT). Important issues such as downward continuation, interpolation methods, and. regularization approaches are also discussed. To demonstrate the feasibility and efficiency of the torus-based semi-analytical approach of gravity field determination in spaceborne gravimetry, disturbing potential data from CHAMP and GRACE and simulated GOCE gravity gradient tensor data are processed.

ASJC Scopus Sachgebiete

Zitieren

Spaceborne gravimetry and gravity field recovery. / Xu, Chen; Weigelt, Matthias; Sideris, Michael G. et al.
in: Canadian Aeronautics and Space Journal, Jahrgang 53, Nr. 3-4, 2007, S. 65-75.

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Xu, C, Weigelt, M, Sideris, MG & Sneeuw, N 2007, 'Spaceborne gravimetry and gravity field recovery', Canadian Aeronautics and Space Journal, Jg. 53, Nr. 3-4, S. 65-75.
Xu, C., Weigelt, M., Sideris, M. G., & Sneeuw, N. (2007). Spaceborne gravimetry and gravity field recovery. Canadian Aeronautics and Space Journal, 53(3-4), 65-75.
Xu C, Weigelt M, Sideris MG, Sneeuw N. Spaceborne gravimetry and gravity field recovery. Canadian Aeronautics and Space Journal. 2007;53(3-4):65-75.
Xu, Chen ; Weigelt, Matthias ; Sideris, Michael G. et al. / Spaceborne gravimetry and gravity field recovery. in: Canadian Aeronautics and Space Journal. 2007 ; Jahrgang 53, Nr. 3-4. S. 65-75.
Download
@article{579cf599bf184cf9b059158aaf6180b0,
title = "Spaceborne gravimetry and gravity field recovery",
abstract = "As an integrated signal of mass transition and distribution, the Earth's gravity senses the inner and outer mass balance of the Earth. However, gravity cannot be measured directly in space but can be derived from other measurements obtained by space vehicles. The dedicated gravity field satellite missions CHAMP, GRACE, and GOCE serve as spaceborne gravimeters by utilizing satellite-to-satellite tracking (SST) and satellite gravity gradiometry (SGG) techniques. In this {"}decade of the geopotentials{"}, these missions will serve different purposes with particular spatial and spectral resolutions. This paper introduces the usefulness of these missions, their impacts on the geosciences, the measurement principles, and their implementations. These space sensors will provide a significant number of observations during their mission lifespans. Therefore, global gravity field recovery is a computationally demanding task. Several approaches aimed at this goal are discussed, namely the brute-force approach, the space-wise approach, the time-wise approach, and the proposed torus-based semi-analytical approach. The paper addresses the characteristics of each approach and focuses mainly on the torus-based semi-analytical approach, which can be used to derive the gravity field from, any geopotential functional. In this approach, the structure of the normal matrix becomes block-diagonal, which leads to a powerful and efficient recovery tool through the use of the fast Fourier transform (FFT). Important issues such as downward continuation, interpolation methods, and. regularization approaches are also discussed. To demonstrate the feasibility and efficiency of the torus-based semi-analytical approach of gravity field determination in spaceborne gravimetry, disturbing potential data from CHAMP and GRACE and simulated GOCE gravity gradient tensor data are processed.",
author = "Chen Xu and Matthias Weigelt and Sideris, {Michael G.} and Nico Sneeuw",
year = "2007",
language = "English",
volume = "53",
pages = "65--75",
number = "3-4",

}

Download

TY - JOUR

T1 - Spaceborne gravimetry and gravity field recovery

AU - Xu, Chen

AU - Weigelt, Matthias

AU - Sideris, Michael G.

AU - Sneeuw, Nico

PY - 2007

Y1 - 2007

N2 - As an integrated signal of mass transition and distribution, the Earth's gravity senses the inner and outer mass balance of the Earth. However, gravity cannot be measured directly in space but can be derived from other measurements obtained by space vehicles. The dedicated gravity field satellite missions CHAMP, GRACE, and GOCE serve as spaceborne gravimeters by utilizing satellite-to-satellite tracking (SST) and satellite gravity gradiometry (SGG) techniques. In this "decade of the geopotentials", these missions will serve different purposes with particular spatial and spectral resolutions. This paper introduces the usefulness of these missions, their impacts on the geosciences, the measurement principles, and their implementations. These space sensors will provide a significant number of observations during their mission lifespans. Therefore, global gravity field recovery is a computationally demanding task. Several approaches aimed at this goal are discussed, namely the brute-force approach, the space-wise approach, the time-wise approach, and the proposed torus-based semi-analytical approach. The paper addresses the characteristics of each approach and focuses mainly on the torus-based semi-analytical approach, which can be used to derive the gravity field from, any geopotential functional. In this approach, the structure of the normal matrix becomes block-diagonal, which leads to a powerful and efficient recovery tool through the use of the fast Fourier transform (FFT). Important issues such as downward continuation, interpolation methods, and. regularization approaches are also discussed. To demonstrate the feasibility and efficiency of the torus-based semi-analytical approach of gravity field determination in spaceborne gravimetry, disturbing potential data from CHAMP and GRACE and simulated GOCE gravity gradient tensor data are processed.

AB - As an integrated signal of mass transition and distribution, the Earth's gravity senses the inner and outer mass balance of the Earth. However, gravity cannot be measured directly in space but can be derived from other measurements obtained by space vehicles. The dedicated gravity field satellite missions CHAMP, GRACE, and GOCE serve as spaceborne gravimeters by utilizing satellite-to-satellite tracking (SST) and satellite gravity gradiometry (SGG) techniques. In this "decade of the geopotentials", these missions will serve different purposes with particular spatial and spectral resolutions. This paper introduces the usefulness of these missions, their impacts on the geosciences, the measurement principles, and their implementations. These space sensors will provide a significant number of observations during their mission lifespans. Therefore, global gravity field recovery is a computationally demanding task. Several approaches aimed at this goal are discussed, namely the brute-force approach, the space-wise approach, the time-wise approach, and the proposed torus-based semi-analytical approach. The paper addresses the characteristics of each approach and focuses mainly on the torus-based semi-analytical approach, which can be used to derive the gravity field from, any geopotential functional. In this approach, the structure of the normal matrix becomes block-diagonal, which leads to a powerful and efficient recovery tool through the use of the fast Fourier transform (FFT). Important issues such as downward continuation, interpolation methods, and. regularization approaches are also discussed. To demonstrate the feasibility and efficiency of the torus-based semi-analytical approach of gravity field determination in spaceborne gravimetry, disturbing potential data from CHAMP and GRACE and simulated GOCE gravity gradient tensor data are processed.

UR - http://www.scopus.com/inward/record.url?scp=44449130127&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:44449130127

VL - 53

SP - 65

EP - 75

JO - Canadian Aeronautics and Space Journal

JF - Canadian Aeronautics and Space Journal

SN - 0008-2821

IS - 3-4

ER -

Von denselben Autoren