@Article{SanchezPradYoko:2014:QuOr,
author = "Sanchez, Diogo Merguizo and Prado, Antonio Fernando Bertachini de
Almeida and Yokoyama, T.",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Universidade Estadual
Paulista (UNESP)}",
title = "On the effects of each term of the geopotential perturbation along
the time I: Quasi-circular orbits",
journal = "Advances in Space Research",
year = "2014",
volume = "54",
number = "6",
pages = "1008--1018",
keywords = "Geodetic satellites, Harmonic analysis, Space flight, China-brazil
earth resources satellites, Computational effort, Direct solar
radiation, Geopotential perturbations, Geopotentials, Mean squared
error, Orbital mechanics, Satellite orbit, Orbits.",
abstract = "This paper provides a useful new method to determine minimum and
maximum range of values for the degree and order of the
geopotential coefficients required for simulations of orbits of
satellites around the Earth. The method consists in a time
integration of the perturbing acceleration coming from each
harmonic of the geopotential during a time interval T. More
precisely, this integral represents the total velocity
contribution of a specific harmonic during the period T.
Therefore, for a pre-fixed minimum contribution, for instance
1×10-8 m/s during the period of time T, any harmonic whose
contribution is below this value can, safely, be neglected. This
fact includes some constraints in the degree and order of the
terms which are present in the geopotential formula, saving
computational efforts compared to the integration of the full
model. The advantage of this method is the consideration of other
perturbations in the dynamics (we consider the perturbations of
the Sun, the Moon, and the direct solar radiation pressure with
eclipses), since these forces affect the value of the perturbation
of the geopotential, because these perturbations depend on the
trajectory of the spacecraft, that is dependent on the dynamical
model used. In this paper, we work with quasi-circular orbits and
we present several simulations showing the bounds for the maximum
degree and order (M) that should be used in the geopotential for
different situations, e. g., for a satellite near 500 km of
altitude (like the GRACE satellites at the beginning of their
mission) we found 35dMd198 for T=1 day. We analyzed the individual
contribution of the second order harmonic (J2) and we use its
behavior as a parameter to determine the lower limit of the number
of terms of the geopotential model. In order to test the accuracy
of our truncated model, we calculate the mean squared error
between this truncated model and the {"} full{"} model, using the
CBERS (China-Brazil Earth Resources Satellite) satellite in this
test. © 2014 COSPAR. Published by Elsevier Ltd. All rights
reserved.",
doi = "10.1016/j.asr.2014.06.003",
url = "http://dx.doi.org/10.1016/j.asr.2014.06.003",
issn = "0273-1177 and 1879-1948",
label = "scopus 2014-11 SanchezPradYoko:2014:QuOr",
language = "en",
urlaccessdate = "27 abr. 2024"
}