A new tool for satellite re-entry predictions
A new tool for satellite re-entry predictions
Satellite drag data plays an important role in the estimation of atmospheric density and the study of thermospheric cooling and contraction. There are many ways of calculating atmospheric density, but inferring thermospheric density from satellite drag data is a relatively cost-effective way of gathering in-situ measurements. Given an initial satellite orbit, one approach is to use an orbital propagator to predict the satellite’s state at some time ahead and then to compare that state with the Two-Line Element (TLE) data at the same epoch. The difference between the mean motions from consecutive TLE sets is calculated then compared to results obtained from the orbital propagator. From this an estimate of global average density can then be calculated. The validation of a new orbital propagator that will be used for this purpose is the primary focus of this paper. Here, the validation takes the form of re-entry prediction for decaying satellites.
Saunders, A.
f42b40b5-5e67-47e2-bde0-0942211201f4
Lewis, H.G.
e9048cd8-c188-49cb-8e2a-45f6b316336a
Swinerd, G.G.
4aa174ec-d08c-4972-9986-966e17e072a0
September 2009
Saunders, A.
f42b40b5-5e67-47e2-bde0-0942211201f4
Lewis, H.G.
e9048cd8-c188-49cb-8e2a-45f6b316336a
Swinerd, G.G.
4aa174ec-d08c-4972-9986-966e17e072a0
Saunders, A., Lewis, H.G. and Swinerd, G.G.
(2009)
A new tool for satellite re-entry predictions.
Fifth European Conference on Space Debris, Darmstadt, Germany.
29 Mar - 01 Apr 2009.
6 pp
.
Record type:
Conference or Workshop Item
(Poster)
Abstract
Satellite drag data plays an important role in the estimation of atmospheric density and the study of thermospheric cooling and contraction. There are many ways of calculating atmospheric density, but inferring thermospheric density from satellite drag data is a relatively cost-effective way of gathering in-situ measurements. Given an initial satellite orbit, one approach is to use an orbital propagator to predict the satellite’s state at some time ahead and then to compare that state with the Two-Line Element (TLE) data at the same epoch. The difference between the mean motions from consecutive TLE sets is calculated then compared to results obtained from the orbital propagator. From this an estimate of global average density can then be calculated. The validation of a new orbital propagator that will be used for this purpose is the primary focus of this paper. Here, the validation takes the form of re-entry prediction for decaying satellites.
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Published date: September 2009
Venue - Dates:
Fifth European Conference on Space Debris, Darmstadt, Germany, 2009-03-29 - 2009-04-01
Organisations:
Astronautics Group
Identifiers
Local EPrints ID: 68971
URI: http://eprints.soton.ac.uk/id/eprint/68971
PURE UUID: 437dc711-d1d0-4efb-acc0-d10251af5e9e
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Date deposited: 13 Oct 2009
Last modified: 26 Jul 2022 01:35
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Contributors
Author:
A. Saunders
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