UPPER ATMOSPHERIC DENSITIES DERIVED FROM STARSHINE SPACECRAFT ORBITS

Similar documents
Lab #8 NEUTRAL ATMOSPHERE AND SATELLITE DRAG LAB

Results from the Atmospheric Neutral Density Experiment Risk Reduction Mission

COUNTING DOWN TO THE LAUNCH OF POPACS

Accuracy of Earth s Thermospheric Neutral Density Models

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

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

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

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

ORBITAL DECAY PREDICTION AND SPACE DEBRIS IMPACT ON NANO-SATELLITES

Calculated and observed climate change in the thermosphere, and a prediction for solar cycle 24

HYPER Industrial Feasibility Study Final Presentation Orbit Selection

Atmospheric density calibration using satellite drag observations

Comparison Of Atmospheric Density Models in the Thermospheric Region: MSIS-86 and DTM-78

Lecture 2c: Satellite Orbits

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

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

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

Orbit Design Marcelo Suárez. 6th Science Meeting; Seattle, WA, USA July 2010

Experimental Analysis of Low Earth Orbit Satellites due to Atmospheric Perturbations

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

A long-term data set of globally averaged thermospheric total mass density

Recurrent Geomagnetic Activity Driving a Multi-Day Response in the Thermosphere and Ionosphere

MAE 180A: Spacecraft Guidance I, Summer 2009 Homework 2 Due Tuesday, July 14, in class.

Orbits in Geographic Context. Instantaneous Time Solutions Orbit Fixing in Geographic Frame Classical Orbital Elements

PRELIMINARY RESULTS TO SUPPORT EVIDENCE OF THERMOSPHERIC CONTRACTION

Ionosphere-Thermosphere Basics - I Neutral Atmosphere Vertical Structure

AS3010: Introduction to Space Technology

Chapter 2: Orbits and Launching Methods

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

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

ORBIT PERTURBATION ANALYSIS OF WEST FORD NEEDLES CLUSTERS

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

New Satellite Drag Modeling Capabilities

EFFECTS OF DIRECT AND INDIRECT SOLAR RADIATION PRESSURE IN ORBITAL PARAMETERS OF GPS SATELITTES

Chapter 2 Empirical Modelling of the Thermosphere

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

Orbit and Transmit Characteristics of the CloudSat Cloud Profiling Radar (CPR) JPL Document No. D-29695

SPCE 5065 Spacecraft Interactions Project 28 August Douglas Hine

PHYSICS 1030 Homework #9

PERFORMANCES OF ATMOSPHERIC DENSITY MODELS DURING SATELLITE REENTRY PREDICTION CAMPAIGNS AT SUNSPOT MINIMUM

NAVIGATION & MISSION DESIGN BRANCH

Stephen H. Knowles Integrity Applications, Inc. Chantilly, VA apps.com

COUNTING DOWN TO THE LAUNCH OF POPACS (POLAR ORBITING PASSIVE ATMOSPHERIC CALIBRATION SPHERES)

Seminar 3! Precursors to Space Flight! Orbital Motion!

Spacecraft De-Orbit Point Targeting using Aerodynamic Drag

FORMATION FLYING WITH SHEPHERD SATELLITES NIAC Fellows Meeting Michael LaPointe Ohio Aerospace Institute

INTERNAL THALES ALENIA SPACE

13 th AAS/AIAA Space Flight Mechanics Meeting

Joule heating and nitric oxide in the thermosphere, 2

AN INVESTIGATION INTO SATELLITE DRAG MODELING PERFORMANCE. Stephen Russell Mance

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

Fundamentals of Astrodynamics and Applications

Satellite Communications

Satellite Orbital Maneuvers and Transfers. Dr Ugur GUVEN

Relative Orbital Elements: Theory and Applications

APPENDIX B SUMMARY OF ORBITAL MECHANICS RELEVANT TO REMOTE SENSING

Earth-Centered, Earth-Fixed Coordinate System

Where Space Begins: Revisiting the Karman Line. Jonathan McDowell

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

Dilution of Disposal Orbit Collision Risk for the Medium Earth Orbit Constellations

PHYSICS 1030 Homework #9

Optimization of Orbital Transfer of Electrodynamic Tether Satellite by Nonlinear Programming

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

Sensitivity of equatorial mesopause temperatures to the 27-day solar cycle

Orbital Debris Observation via Laser Illuminated Optical Measurement Techniques

THERMOSPHERE DENSITY CALIBRATION IN THE ORBIT DETERMINATION OF ERS-2 AND ENVISAT

Comparison between the KOMPSAT-1 drag derived density and the MSISE model density during strong solar and/or geomagnetic activities

Satellite meteorology

The Orbit Control of ERS-1 and ERS-2 for a Very Accurate Tandem Configuration

Experiment Design and Performance. G. Catastini TAS-I (BUOOS)

Creating Satellite Orbits

The solar and geomagnetic inputs into the JB2008 thermospheric density model for use by CIRA08 and ISO 14222!

1 A= one Angstrom = 1 10 cm

PW-Sat two years on orbit.

REVIEW OF RESULTS ON ATMOSPHERIC DENSITY CORRECTIONS 1

Celestial Mechanics and Satellite Orbits

Figure 1. View of ALSAT-2A spacecraft

Solar EUV and XUV energy input to thermosphere on solar rotation time scales derived from photoelectron observations.

Orbit Definition. Reference Vector. Vernal (March) Equinox Vector. Sun Vector

CHAPTER 3 PERFORMANCE

FORECASTING OF SPACE ENVIRONMENT PARAMETERS FOR SATELLITE AND GROUND SYSTEM OPERATIONS. W. Kent Tobiska a

Lecture 1d: Satellite Orbits

Analytical Method for Space Debris propagation under perturbations in the geostationary ring

EVALUATION OF A SPACECRAFT TRAJECTORY DEVIATION DUE TO THE LUNAR ALBEDO

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

ASTRIUM. Interplanetary Path Early Design Tools at ASTRIUM Space Transportation. Nathalie DELATTRE ASTRIUM Space Transportation.

Atmospheric escape. Volatile species on the terrestrial planets

Trends in the middle atmosphere from ground based sensors at mid and high latitudes

Geometry of Earth Sun System

Fundamentals of Satellite technology

A.I. Nazarenko 1

SECTION 9 ORBIT DATA - LAUNCH TRAJECTORY

A non-linear simulator written in C for orbital spacecraft rendezvous applications.

ATTITUDE CONTROL MECHANIZATION TO DE-ORBIT SATELLITES USING SOLAR SAILS

Effect of the altitudinal variation of the gravitational acceleration on the thermosphere simulation

RAPID GEOSYNCHRONOUS TRANSFER ORBIT ASCENT PLAN GENERATION. Daniel X. Junker (1) Phone: ,

arxiv: v1 [astro-ph.ep] 23 May 2018

MULTI PURPOSE MISSION ANALYSIS DEVELOPMENT FRAMEWORK MUPUMA

An Optical Survey for Space Debris on Highly Eccentric MEO Orbits

North Korea Satellite Launch

Transcription:

UPPER ATMOSPHERIC DENSITIES DERIVED FROM STARSHINE SPACECRAFT ORBITS R. G. Moore 1, J. Lean 2, J. M. Picone 2, S. Knowles, A. Hedin 2, and J. Emmert 2 1. 855 Sierra Vista Road, Monument CO 8012 2. Naval Research Laboratory, Washington DC 2075. Raytheon Company, Lexington MA 02421 Motivation - improved density model for orbit tracking Starshine Orbits - cycle 2 max Spacecraft Drag - independent data for model validation Starshine vs NRLMSIS model density comparison

Upper Atmosphere Density Causes Spacecraft Drag drag acceleration = 0.5 ρ v 2 C d A/ M ρ v C d A atmospheric density velocity relative to local environment drag coefficient, M mass cross sectional area perpendicular to velocity vector three Starshine Spacecraft with spherical geometry and known mass have been launched into circular low-earth orbits 9,000 resident space objects larger than 15 cm

Starshine Spacecraft 1 2 Properties of Starshine Spacecraft Launch 1999 05-27 2001 12-05 2001 09-29 Eccentricity Reentry 2000 02-18 2002 05-01 200 01-21 Initial Altitude (km) 85 70 475 0.001 0.002 0.001 Inclination (degree) 51.6 51.6 67 Mass (kg) 9 8 90 Diameter (cm) 48 (19 ) 48 (19 ) 94 (7 ) C D 2.1 2.1 2.1 Inverse Ballistic Coefficient (cm 2 gm -1 ) 0.097 0.100 0.162

Solar Activity Alters Temperature and Composition at Starshine Altitudes Temperature Primary Constituents solar min dashed F 10.7 =70, <F 10.7 > 81 =70, Ap=11 solar max - solid F 10.7 =200, <F 10.7 > 81 =174, Ap=11

Starshine Two Line Element Sets USSPACECOM orbit parameters derived from General Perturbation theory: six Kozai mean elements inclination right ascension of ascending node argument of perigree eccentricity mean motion mean anomaly plus drag (Bstar) 10 - provided by Dr T. Kelso, http://www.celestrak.com

Atmospheric Density Derived from TLEs instantaneous change in mean motion with time dn = 1/ 2 / n µ BFρv 2 dt change in mean motion between two successive TLE epochs density average between two successive TLE epochs n = mean motion, t = time ρ = mass density B = inverse ballistic coef = C d A/M µ = GM, gravitational parameter v = spacecraft velocity F = wind factor rω cos( ) 2 1 i v n ρ n 1/ 2 / 2 1 ne µ Bρ 2 E E = 2 ( n n ) µ 2 1 1/ Bn ρ = E Fρv E Fv 2 / Fv dt dt Fv dt dt where ρ E and n E are effective values between two successive TLE epochs:

Starshine Orbits are Assumed Circular for circular orbits Fv dt = Fv ( t t ) 2 1 density at TLE epoch ρ 2 / 2 dn µ 1/ dt Bn v F gravitational constant wind factor derivative of mean motion inverse ballistic mean motion speed coefficient height and speed are approximately constant during Starshine orbits so Fv dt Fv ( t t ) 2 1

Quantities for Drag Calculations obtained from TLE s directly obtained from SPG4 with TLE inputs obtained from SPG4 and TLE s

Total Mass Densities Derived from Drag on Starshine Spacecraft

Starshine Total Mass Densities and US Standard Atmosphere (1976) Densities from Starshine drag: higher than USSA76 at altitudes above 200 km lower than USSA76 at altitudes below 200 km Starshine 1,2 & orbits occurred during overall high solar activity

NRL s Time-Dependent Upper Atmosphere Density Specification Model calculates upper atmosphere total mass density, composition and temperature, for specified altitude, latitude, longitude, local time, day of year and solar activity NRLMSIS-00 Naval Research Laboratory Mass Spectrometer and Incoherent Scatter Model (2000) enhanced, revised model within MSIS framework - Hedin, 1987, 1991 extended database for model formulation - total mass densities from satellite - excluding Starshine accelerometers and orbit determinations - temperatures from incoherent scatter radar -O 2 densities from solar UV occultation solar/geomagnetic inputs -F 10.7, F 10.7 A, Ap Picone et al., Phys. Chem. of Earth, 2000

Comparison of Starshine and NRLMSIS Total Mass Densities NRLMSIS model is evaluated around one complete Starshine orbit 1 2 orbit-average model density is compared with Starshine drag value Starshine 2 & show similar differences with NRLMSIS

NRLMSIS Total Mass Density Variations During Single Starshine Orbits Starshine location around orbit input to NRLMSIS model, with specified dayof-year and solar activity density calculated by NRLMSIS model

Starshine and NRLMSIS Differences related to solar indices SOHO EIT EUV/04 Å 0JUL99 14AUG99 Starshine 1 when NRLMSIS densities lead Starshine densities, F10.7 coronal index leads chromospheric index (derived from ratios of core-to-wing emission in solar Ca II K and Mg II h&k Fraunhofer lines) exponential fall off differences between NRLMSIS and Starshine densities track differences between F10.7 and chromospheric indices

F 10.7, [F 10.7 ] 81 A P Reformulating NRLMSIS Upper Atmosphere Density Model Current Version: NRLMSIS-00 -- proxies for EUV radiation -- proxy for geomagnetic effect of solar wind Picone et al., Phys. Chem. of the Earth, Part C, 2000, Picone et al., JGR, in preparation I CHROM, [I CHROM ] 81 A P Future Version: NRLMSIS-SOLC SOLC -- proxies for EUV radiation -- proxy for geomagnetic effect of solar wind NRLMSIS has been reformulated using a new solar irradiance index - improvements will be assessed by comparisons with Starshine drag

SUMMARY: Upper Atmospheric Densities Derived From Starshine Spacecraft Orbits mass densities at 10-470 km derived from USSPACECOM TLEs along Starshine 1,2, orbits densities have solar EUV induced 27-day variations superimposed on exponential fall-off with altitude Starshine and NRLMSIS-00 densities agree to within 20% differences between chromospheric and F 10.7 proxies may account for some of the differences NRLMSIS has been reformulated with a new solar EUV proxy NRLMSIS-SOLC Starshine 4, 5 are in progress model validation during 11-year solar cycle comparisons with TIMED irradiance & density

Starshine Spacecraft Series tracking the 11-year solar activity cycle Starshine 1, STS-96, mid-1999, 85 km, 9 kg Starshine, Kodiak, Sept 2001, 471 km, 90 kg Starshine 2, STS-108, Dec 2001, 87 km, 8 kg Starshine 4,5, TBD 85 km TIMED: GUVI atmospheric densities SEE solar EUV irradiances