Aerodynamic Lift and Drag Effects on the Orbital Lifetime Low Earth Orbit (LEO) Satellites

Similar documents
ORBITAL DECAY PREDICTION AND SPACE DEBRIS IMPACT ON NANO-SATELLITES

Propagation of Forecast Errors from the Sun to LEO Trajectories: How Does Drag Uncertainty Affect Conjunction Frequency?

PRELIMINARY RESULTS TO SUPPORT EVIDENCE OF THERMOSPHERIC CONTRACTION

Experimental Analysis of Low Earth Orbit Satellites due to Atmospheric Perturbations

ATTITUDE CONTROL MECHANIZATION TO DE-ORBIT SATELLITES USING SOLAR SAILS

AS3010: Introduction to Space Technology

Optimization of Orbital Transfer of Electrodynamic Tether Satellite by Nonlinear Programming

How CubeSats are Helping Address the Space Debris Problem: Results from the Polar Orbiting Passive Atmospheric Calibration Spheres

AN ANALYTICAL SOLUTION TO QUICK-RESPONSE COLLISION AVOIDANCE MANEUVERS IN LOW EARTH ORBIT

Extending the Patched-Conic Approximation to the Restricted Four-Body Problem

Statistical methods to address the compliance of GTO with the French Space Operations Act

ABSTRACT. Nomenclature

COE CST Fifth Annual Technical Meeting. Space Environment MMOD Modeling and Prediction. Sigrid Close and Alan Li Stanford University

AST111, Lecture 1b. Measurements of bodies in the solar system (overview continued) Orbital elements

Analytical Non-Linear Uncertainty Propagation: Theory And Implementation

Spacecraft De-Orbit Point Targeting using Aerodynamic Drag

1. (a) Describe the difference between over-expanded, under-expanded and ideallyexpanded

Fundamentals of Astrodynamics and Applications

Ulrich Walter. Astronautics. The Physics of Space Flight. 2nd, Enlarged and Improved Edition

Lab #8 NEUTRAL ATMOSPHERE AND SATELLITE DRAG LAB

UPPER ATMOSPHERIC DENSITIES DERIVED FROM STARSHINE SPACECRAFT ORBITS

Section 13. Orbit Perturbation. Orbit Perturbation. Atmospheric Drag. Orbit Lifetime

Optimal Gravity Assisted Orbit Insertion for Europa Orbiter Mission

Atmospheric Drag. Modeling the Space Environment. Manuel Ruiz Delgado. European Masters in Aeronautics and Space

Orbital Debris Observation via Laser Illuminated Optical Measurement Techniques

Analytical Non-Linear Uncertainty Propagation: Theory And Implementation

An Analysis of N-Body Trajectory Propagation. Senior Project. In Partial Fulfillment. of the Requirements for the Degree

Universal Gravitation

A Senior Project. presented to. the Faculty of the Aerospace Engineering Department. California Polytechnic State University, San Luis Obispo

COVARIANCE DETERMINATION, PROPAGATION AND INTERPOLATION TECHNIQUES FOR SPACE SURVEILLANCE. European Space Surveillance Conference 7-9 June 2011

Astrodynamics (AERO0024)

HYPER Industrial Feasibility Study Final Presentation Orbit Selection

Chapter 13. Universal Gravitation

Chapter 13. Gravitation

Astrodynamics (AERO0024)

APPENDIX B SUMMARY OF ORBITAL MECHANICS RELEVANT TO REMOTE SENSING

ACCURACY ASSESSMENT OF GEOSTATIONARY-EARTH-ORBIT WITH SIMPLIFIED PERTURBATIONS MODELS

MARYLAND U N I V E R S I T Y O F. The Space Environment. Principles of Space Systems Design

Satellite Orbital Maneuvers and Transfers. Dr Ugur GUVEN

Astromechanics. 10. The Kepler Problem

Space Travel on a Shoestring: CubeSat Beyond LEO

The Space Environment

Long-Term Evolution of High Earth Orbits: Effects of Direct Solar Radiation Pressure and Comparison of Trajectory Propagators

Space Surveillance with Star Trackers. Part II: Orbit Estimation

Study of Required Thrust Profile Determination of a Three Stages Small Launch Vehicle

ORBIT PERTURBATION ANALYSIS OF WEST FORD NEEDLES CLUSTERS

5.12 The Aerodynamic Assist Trajectories of Vehicles Propelled by Solar Radiation Pressure References...

EXAMINATION OF THE LIFETIME, EVOLUTION AND RE-ENTRY FEATURES FOR THE "MOLNIYA" TYPE ORBITS

Design and Analysis of Satellite Orbits for the Garada Mission

PLANETARY ORBITAL DYNAMICS (PLANODYN) SUITE FOR LONG TERM PROPAGATION IN PERTURBED ENVIRONMENT. Camilla Colombo 1

Estimating the Error in Statistical HAMR Object Populations Resulting from Simplified Radiation Pressure Modeling

Chapter 2: Orbits and Launching Methods

Design of Orbits and Spacecraft Systems Engineering. Scott Schoneman 13 November 03

Lecture D30 - Orbit Transfers

SUN INFLUENCE ON TWO-IMPULSIVE EARTH-TO-MOON TRANSFERS. Sandro da Silva Fernandes. Cleverson Maranhão Porto Marinho

PHYS 101 Previous Exam Problems. Gravitation

Satellite Communications

The Cosmic Perspective Seventh Edition. Making Sense of the Universe: Understanding Motion, Energy, and Gravity. Chapter 4 Lecture

EFFECT OF DENSITY MODEL TIME-DELAY ERRORS ON ORBIT PREDICTION

AUTONOMOUS AND ROBUST RENDEZVOUS GUIDANCE ON ELLIPTICAL ORBIT SUBJECT TO J 2 PERTURBATION.

Feedback Control of Spacecraft Rendezvous Maneuvers using Differential Drag

Satellite Re-entry Modeling and Uncertainty Quantification. Matthew Horsley Lawrence Livermore National Laboratory

Negating the Yearly Eccentricity Magnitude Variation of Super-synchronous Disposal Orbits due to Solar Radiation Pressure

ORBITS WRITTEN Q.E. (June 2012) Each of the five problems is valued at 20 points. (Total for exam: 100 points)

Orbital and Celestial Mechanics

(2012) ISSN

Past and Future Climate of Thermospheric Density: Solar and Anthropogenic Influences

Using Differential Aerodynamic Forces for CubeSat Orbit Control Sanny R. Omar

CHAPTER 3 PERFORMANCE

Chapter 4 Making Sense of the Universe: Understanding Motion, Energy, and Gravity. Copyright 2009 Pearson Education, Inc.

Infrared Earth Horizon Sensors for CubeSat Attitude Determination

Circular vs. Elliptical Orbits for Persistent Communications

Infrared Earth Horizon Sensors for CubeSat Attitude Determination

Strathprints Institutional Repository

Study of the Fuel Consumption for Station-Keeping Maneuvers for GEO satellites based on the Integral of the Perturbing Forces over Time

Copyright 2010 Pearson Education, Inc. GRAVITY. Chapter 12

Chapter 12 Gravity. Copyright 2010 Pearson Education, Inc.

4.1 Describing Motion. How do we describe motion? Chapter 4 Making Sense of the Universe: Understanding Motion, Energy, and Gravity

AP Physics C Textbook Problems

Chapter 8 Part 1. Attitude Dynamics: Disturbance Torques AERO-423

NUMERICAL SEARCH OF BOUNDED RELATIVE SATELLITE MOTION

TAU Extensions for High Enthalpy Flows. Sebastian Karl AS-RF

A = 6561 times greater. B. 81 times greater. C. equally strong. D. 1/81 as great. E. (1/81) 2 = 1/6561 as great Pearson Education, Inc.

Analysis of the Briz-M Propellant Tank (35698) Fragmentation Using the Velocity Perturbations of the Fragments

Lecture 2c: Satellite Orbits

EVALUATION OF A SPACECRAFT TRAJECTORY DEVIATION DUE TO THE LUNAR ALBEDO

Chapter 12 Gravity. Copyright 2010 Pearson Education, Inc.

NAVIGATION & MISSION DESIGN BRANCH

Chapter 13. Gravitation

Orbital Anomaly Detection and Application of Space Object

Satellite meteorology

PHYSICS. Chapter 13 Lecture FOR SCIENTISTS AND ENGINEERS A STRATEGIC APPROACH 4/E RANDALL D. KNIGHT Pearson Education, Inc.

SCIENCE & TECHNOLOGY

ORBITAL CHARACTERISTICS DUE TO THE THREE DIMENSIONAL SWING-BY IN THE SUN-JUPITER SYSTEM

orbits Moon, Planets Spacecrafts Calculating the and by Dr. Shiu-Sing TONG

Previous Lecture. The Von Zeipel Method. Application 1: The Brouwer model. Application 2: The Cid-Lahulla model. Simplified Brouwer transformation.

Motion of Satellite under the Effect of Oblateness of Earth and Atmospheric Drag arxiv: v3 [physics.space-ph] 29 Jan 2019

Lecture 19: The Moon & Mercury. The Moon & Mercury. The Moon & Mercury

4.1 Describing Motion

Chapter 5 - Part 1. Orbit Perturbations. D.Mortari - AERO-423

Transcription:

Aerodynamic Lift and Drag Effects on the Orbital Lifetime Low Earth Orbit (LEO) Satellites I. Introduction Carlos L. Pulido Department of Aerospace Engineering Sciences University of Colorado Boulder Abstract The effects of aerodynamic perturbation forces on the orbital life of low altitude Low Earth Orbit (LEO) satellites are investigated, with a focus on the secular perturbations caused by lift and drag. The secular effects can be divided into the circularization of the orbit for both lift and drag perturbation forces, and the decrease of the orbit semimajor axis for drag perturbation. A study of these effects on an attitude stabilized satellite with an orbit of initial perigee altitude of 300 km and initial eccentricity of 0.12 is performed. The objective is to determine whether the effects of aerodynamic forces (i.e., lift and drag) can be effectively used to control the orbital lifetime of a satellite. a. Background The analysis of a satellite s motion around the Earth can be approximated by assuming a Keplerian orbit, where Earth is assumed to be a perfect sphere with a mass much greater than that of the satellite, and where gravity is the only force acting on the orbiting body [1]. The actual motion of the satellite is then perturbed from this reference orbit by other external forces, such as aerodynamic forces, solar radiation pressure and non-spherical mass effects [2]. In low-earth orbits

(LEO) the second major perturbation force acting on a satellite is aerodynamic drag. To a lesser extent, the aerodynamic lift force may also perturb the orbit of the satellite if it is attitude stabilized. These forces play a major role into a satellite s orbital life and eventual decay. For LEO missions of perigee altitudes of less than 500 km, the secular effects due to aerodynamic forces are of great importance as the orbital lifetime has to be long enough to satisfy mission requirements [3]. b. Foundation At low altitude LEO orbits, aerodynamic forces are the principal non-gravitational forces acting on a satellite. The aerodynamic drag acceleration, f D, is defined in Equation 1, where ρ is the atmospheric density, is the coefficient of drag, A is the cross-sectional area, m is the mass of the satellite and V is the magnitude of the velocity. Drag acts opposite to the velocity vector and continuously slows down and removes energy from the satellite [3]. Aerodynamic lift acceleration, f L, acts perpendicular to the velocity vector and is defined in Equation 2, where ρ is the atmospheric density, is the coefficient of lift, A is the cross-sectional area, m is the mass of the satellite and V is the magnitude of the velocity. Lift is mainly achieved through the use of lifting surfaces, such as airfoils. These forces are highly dependent on the atmospheric density (varies with altitude and epoch) and the cross-sectional area normal to the velocity vector (varies with attitude) [3]. To better understand the aerodynamic forces acting on a satellite, the flow of atmospheric air around the satellite has to be characterized. At very low altitudes, the density of the atmospheric air is high enough to consider the air flow a continuum or

bulk of air particles moving over a body. However, at altitudes above 75 km the flow of air cannot be assumed to be a continuum as the mean free path, λ,between air molecules becomes large (on the order of 1cm), and kinetic theory of gases has to be used instead to describe the airflow [4]. The Aerodynamic drag has an appreciable effect up to an altitude of around 1000 km, where there is a lack of collisions between the satellite s surface and air molecules [4]. Similarly, the aerodynamic lift only has a significant effect on the orbit for perigee altitudes up to 500 km [5]. The presence of the aerodynamic forces in LEO, will cause perturbations to the Keplerian orbital elements. These perturbations can be categorized as secular (i.e., non-periodic), long period (i.e., longer than the orbit s period), or short period (i.e., shorter than the orbit s period) [1]. Most of the satellites will exhibit a constant tumbling or rotational motion during the period of their orbit, which will cause the lift vector that acts normal to the velocity to average out over their life time [5]. For these cases, only the perturbations due to atmospheric drag are considered. However, when a satellite s attitude is stabilized at a particular angle of incidence to the airflow for a long period of the orbit, particularly near the perigee, it is expected that aerodynamic lift will have an effect on the orbit [5]. Figure 1.1 shows the direction of the forces acting on the satellite for this case. The perturbation to the orbital elements will affect the satellite s lifetime and will have to be taken into account for mission planning. This study will focus on the secular perturbations to the orbit caused by aerodynamic lift and drag.

L D V Fig ure 1.1 Dir ecti on of Lift, L, and Dra g, D, forc es wit h resp

ect to the velo city vect or, V, for a gen eric attit ude stab ilize d sate llite. c. Fundamental Concepts The perturbations caused by the aerodynamic forces can be analyzed starting with the equations of motion for a Keplerian orbit and introducing a perturbing acceleration f, as defined by Equation 3, where r is the satellite s position vector and μ is the gravitational parameter [5]. To simplify the initial analysis, only one perturbing force will be analyzed at a given time.

The perturbing forces f D and f L due to lift and drag are defined in Equations 4 and 5. We can define the direction of the perturbing accelerations by introducing the unit vectors P, Q, W from the perifocal coordinate system [3], where P is in the orbital plane in the direction of perigee, W in the direction of the angular momentum vector h, Q is the cross product between P and W. For perturbed motion, the semi-major axis a, the specific angular momentum vector h and Hamilton s integral e are not constant, and their rates of change are defined by [5]: From these equations, we can observe that the perturbing force due to lift will not have an effect in the change in semi-major axis, as it is normal to the velocity vector [5]. In addition, we can see that the perturbing force due to drag will have an effect in both the semi-major axis and the eccentricity. However, to provide a true analysis of the orbit s perturbation the parameters that make up the lift and drag forces have to be understood.

Atmospheric Density The atmospheric density is imperative in the calculations of the aerodynamic forces, yet it is a parameter that varies with altitude and solar activity, principally over the course of a solar cycle. The mean daily F10.7 index of radio flux from the Sun, is a measurement of the radio flux at a wavelength of 10.7 cm in units of 10-22 watts/m 2 /Hz, and is a tool used to determine solar maxima and minima (Figure 1.2) [3]. In addition, to the radio flux index, geomagnetic indices, such as the AP index can be used to model the environment due to solar variations. These variations in solar activity can have a big impact in satellite orbital life. As seen in Wertz, satellites decay very rapidly during solar maxima and very slowly during solar minima [3]. The National Oceanic and Atmospheric Administration is in charge of these measurements, and their values for any particular past day can be found on their website (http://www.noaa.gov). Using this atmospheric information, robust atmospheric models can be used such as the 2001 United States Naval Research Laboratory Mass Spectrometer and Incoherent Scatter Radar Exosphere (NRLMSISE-00 Model 2001), which maps out the atmosphere from sea level to 1000 km [6]. This project will use the NRLMSISE-00 Model 2001 for density calculations.

Fig ure 1.2 Obs erve d dail y mea n radi o flux at 10.7 cm. (http ://va dem ecum.bran denb erger.eu/g rafik en/kl ima/ solar _flux. png)

Coefficients of Lift and Drag The spacecraft s lift and drag coefficients are primarily affected by the satellite s shape, attitude, atmospheric density and surface conditions (i.e., smooth, rough, or sticky) [3]. The surface condition greatly affects the manner which the molecules reflect from the surface of the satellite. Equations 9 through 12 show how the coefficients of lift and drag can be calculated for specular and diffuse cases, with the angle of incidence ψ, surface area S, incoming velocity v i and reflecting velocity v r [3] [7]. The coefficient of lift can be assumed constant over the orbit, or it can vary by the eccentric anomaly [5]. For an eccentric anomaly is negative in the range 0 < E < π, and is positive in the range π < E < 2π. For this project, the coefficient of lift will vary over the orbit and will be calculated using only specular reflection, as described by Equation 10, at an angle of incidence ψ = 45 to match the work done by G.E. Cook [5]. A baseline coefficient of drag C D of 2.2 will be selected, to match the work done by K. Moe and M. Moe [8]. Specular Reflection: Diffuse Reflection: Ballistic Coefficient

The coefficient of drag C D, the cross-sectional area A, and the mass of the satellite m can be combined into a single parameter: the ballistic coefficient β, as defined in Equation 13. Similarly, G.E. Cook defines a parameter Φ, by grouping the absolute value of the coefficient of lift C L, the cross-sectional area A, and the mass of the satellite m, as defined in Equation 14 [5]. Inspection of Equations 13 and 12, show that a satellite with the same cross-sectional area and higher mass will be more resistant to the aerodynamic forces, as expected due to the inertial properties of mass [3]. The area to mass ratio for this project will be 0.01 m 2 /kg, in order to compare to the work performed by G.E. Cook [5]. Secular Perturbations Due to Lift and Drag To find the secular perturbations due to lift and drag, start with the equation of motion of Equation 3, and decomposing the vector equations into can be split into radial, cross-radial, and perpendicular components. This method generates the Gaussian variational equations (GVE). Walter shows that through these equations one can determine that drag will have secular effects on semi-major axis and eccentricity [9]. Through a similar approach, Cook determines that lift will only have secular effect on eccentricity, and will not act once the orbit is circularized [5]. Following the work of Walter and Cook, the decoupled secular effects of lift and drag on the orbit can be found for elliptical and circular orbits, as shown in Equations 15-19 [9] [5]. In these equations, H per is the scale height at the perigee, r per is the radius at perigee and ρ per is the density at the perigee. Elliptic Orbits

For the following equations, an orbit is defined as circular when. The following equations are only valid when this is true. o Secular Effects Caused by Atmospheric Drag ( ) ( ) o Secular Effects Caused by Atmospheric Lift Circular Orbits For the following equations, an orbit is defined as circular when. The following equations are only valid for. o Secular Effects Caused by Atmospheric Drag II. Literature Search

[1] D.A. Vallado, Fundamentals of Astrodynamics and Applications, 3rd. Edition. Hawthorne: Microcosm Press and New York: Springer, 2007. [2] B. Wie, Space Vehicle Dynamics and Control, AIAA, 2008 [3] J. Wertz, Space Mission Engineering: The New SMAD, Microcosm Press, 2011. [4] C. Shen, Rarefied Gas Dynamics: Fundamentals, Simulations and Micro Flows, Springer, 2005. [5] G.E. Cook, The Effect of Aerodynamic Lift on Satellite Orbits, Planetary and Space Science, Vol. 12, pp. 1009-1020, 1964. [6] J. Picone, "NRLMSISE-00: A New Empirical Model of the Atmosphere," 2003. [Online]. Available: http://www.nrl.navy.mil/research/nrl-review/2003/atmosphericscience/picone/. [Accessed 10 12 2012]. [7] P. Moore, The Effect of Aerodynamic Lift on Near Circular Satellite Orbits, Planetary and Space Science, Vol. 33, No. 5, pp. 479-491, 1985. [8] K. Moe and M. Moe, "Gas-Surface Interactions and Satellite Drag Coefficients", Planetary and Space Science, 2005. [9] U. Walter, Astronautics, Wiley-VCH, 2008. [10] M.F. Storz et al., High accuracy satellite drag model (HASDM), Advances in Space Research, Vol 36, Issue 12, 2005. [11] D.G. King-Hele, D.M.C. Walker, Predicting the orbital lifetimes of Earth satellites, Acta Astronautica, Vol. 18, pp. 123-131, 1988. III. Problem of Interest a. Importance of Aspect to the Study The main objective of this study is to assess the how aerodynamic forces perturb the orbit of a satellite and how they affect the orbital lifetime of a satellite in LEO. This section will take a look at how the acceleration due to atmospheric drag circularizes the

orbit of an attitude stabilized satellite in an initial baseline orbit of perigee altitude of 300 km and eccentricity of 0.12. The mission will be flown for three different values of C D, starting with a baseline value of 2.2. The difference in coefficient of drag, will lead to a modification in ballistic coefficient which translates to a different satellite design. The circularization times of these three different designs will be compared. b. Importance of Problem to the Field of Astrodynamics Since aerodynamic forces are the principal non-gravitational forces acting on a satellite at low altitude LEO orbits, it is important to understand how different satellite designs will affect the orbital lifetime. Understanding the rate of orbital decay attributed to atmospheric drag can allow a mission designer to allocate the appropriate propulsion requirements to counter act drag in order for the satellite to stay in orbit for the duration of the mission. This study can also have implications in orbital debris removal, since a mission can be designed to decrease the orbital lifetime of debris taking advantage of the decay due to atmospheric drag. c. Development of Solution Method The following steps are followed in the development of the solution: 1. Initialize all of the orbit parameters for the baseline mission of perigee altitude of 300 km and eccentricity of 0.12, using the information in the Fundamental Concepts section. The satellite will begin its orbit above Boulder, on Jan. 8 th, 2009, and will use this date to calculate the atmospheric data for density calculations. 2. Set the coefficient of drag to the desired value and calculate the ballistic coefficient given the baseline area to mass ratio of 0.01 m 2 /kg. The baseline mission uses a C D of 2.2, and comparison missions use a C D of 3 and 4. 3. Using numerical methods propagate the orbit in time, doing a time step every hour. The secular changes in semi-major axis and eccentricity are calculated at each time step using the equations developed in the Fundamental Concepts

section. The time for circularization is recorded, and the orbital lifetime is estimated. d. Analysis of Method The following circularization times were obtained for the missions using the method described in the Description of the Solution Method Section: Mission Mission I (Baseline) Mission II (C D = 3) Mission III (C D = 4) Time of Circularization 706.9 days 605.3 days 524.3 days It is observed that as the coefficient of drag and ballistic coefficient increase, the time it takes for the elliptic orbit to become circular decreases. This is expected, from the discussion in the Fundamental Concept section. The mission profiles are shown below. Baseline Mission: C D = 2.2

Semi-major axis, km 7600 7500 Circularization of Orbit C D = 2.2 7400 7300 7200 7100 7000 6900 6800 6700 0 200 400 600 800 Time, days

Eccentricity 0.12 0.1 Circularization of Orbit C D = 2.2 0.08 0.06 0.04 0.02 0 0 200 400 600 800 Time, days Mission II: C D = 3

Semi-major axis, km 7600 7500 Circularization of Orbit C D = 3.0 7400 7300 7200 7100 7000 6900 6800 6700 0 100 200 300 400 500 600 700 Time, days

Eccentricity 0.12 Circularization of Orbit C D = 3.0 0.1 0.08 0.06 0.04 0.02 0 0 100 200 300 400 500 600 700 Time, days Mission III: C D = 4

Semi-major axis, km 7600 7500 Circularization of Orbit C D = 4.0 7400 7300 7200 7100 7000 6900 6800 6700 0 100 200 300 400 500 600 Time, days

Eccentricity 0.12 Circularization of Orbit C D = 4.0 0.1 0.08 0.06 0.04 0.02 0 0 100 200 300 400 500 600 Time, days Mission Comparison

Semi-major axis, km 7600 7500 7400 Circularization of Orbit C D = 2.2 C D = 3.0 C D = 4.0 7300 7200 7100 7000 6900 6800 6700 0 200 400 600 800 Time, days

Eccentricity 0.12 0.1 Circularization of Orbit C D = 2.2 C D = 3.0 C D = 4.0 0.08 0.06 0.04 0.02 0 0 200 400 600 800 Time, days Further analysis on the orbital decay of the satellite was planned, but due to numerical problems in the propagation algorithm an analysis of the decay from a circular orbit could not be achieved. The time for circularization, however, does provide some insight on the effects of atmospheric drag on the orbital lifetime. From Walter, we know that the ratio between the time of circularization of an elliptical orbit and the time of circular orbit lifetime is equal to 1.7 [9]. Using this information we can provide an estimate for the total orbital lifetime of the satellites for the missions: Mission Mission I (Baseline) Mission II (C D = 3) Mission III (C D = 4) Estimated Orbital Lifetime 1122.72 days 961.36 days 832.71 days

IV. Extension a. Extension to the Work Presented in the Literature This project will build on the baseline mission, and include the secular perturbations due to aerodynamic lift in addition to the secular perturbation due to drag. Only the baseline case of a coefficient of drag equal to 2.2 will be considered. The time to circularize the orbit will be compared to the case where only the drag is present. This study will make a case to whether the aerodynamic lift is important in the modeling of perturbations to an attitude stabilized satellite in a low LEO orbit. b. Analyze the Extension The following circularization times were obtained for the missions using the method described in the Description of the Solution Method Section: Mission Mission I (Baseline) Extension Mission (Lift Effects) Time of Circularization 706.9 days 460.7 days Adding the secular perturbation due to lift to the baseline mission significantly reduces the time of circularization by 34.82 %. This effect is greater than that exhibited by missions II and III, which increased the coefficient of drag by a significant amount. In addition, looking at the mission profiles below, we can see that the circularization is faster, but the final circular orbit is of greater radius than that of the baseline design. This is an interesting effect that was not expected. Again, due to numerical problems in the propagation algorithm an analysis of the decay from a circular orbit could not be achieved, and is something that should be recommended for future work in order to investigate the larger radius of the final circular orbit.

Baseline Including Aerodynamic Lift Effects

Semi-major axis, km 7600 7550 Circularization of Orbit Lift Perturbation 7500 7450 7400 7350 7300 7250 0 100 200 300 400 500 Time, days

Eccentricity 0.12 Circularization of Orbit Lift Pertubation 0.1 0.08 0.06 0.04 0.02 0 0 100 200 300 400 500 Time, days Comparison with Baseline Mission

Semi-major axis, km 7600 7500 7400 Circularization of Orbit C D = 2.2 Lift Perturbation 7300 7200 7100 7000 6900 6800 6700 0 200 400 600 800 Time, days

Eccentricity 0.12 0.1 Circularization of Orbit C D = 2.2 Lift Pertubation 0.08 0.06 0.04 0.02 0 0 200 400 600 800 Time, days c. Recommendations Based on Analysis From the results above, we can see that including the secular effects due to aerodynamic lift significantly reduces the circularization time. Therefore, based on the analysis it is recommended to include the effects of aerodynamic lift for an attitude stabilized satellite in LEO. V. Summary and Conclusions The effects of aerodynamic perturbation forces on the orbital life of low altitude Low Earth Orbit (LEO) satellites were investigated, with a focus on the secular perturbations caused by lift and drag. The secular effects can be divided into the circularization of the orbit for both lift and drag perturbation forces, and the decrease of the orbit semi-major

axis for drag perturbation. A study of these effects on an attitude stabilized satellite with an orbit of initial perigee altitude of 300 km and initial eccentricity of 0.12 is performed. It was determined that aerodynamic lift does contribute to the orbital decay of the satellite and must be included in the modeling of attitude stabilized satellites. However, further analysis has to be carried out to fully understand these effects, as numerical problems with the algorithm did not allow for an extensive analysis of the subject. From the current analysis, one can infer that a combination of lift and drag secular effects could be used in order to decrease the orbital lifetime of a satellite faster than just increasing the ballistic coefficient. This could prove useful in the field of orbital debris mitigation and collection. MATLAB Source Code PDF Version