Investigation of different flyby geometries for asteroid Steins - Surface area, stereo and phase angle coverage Sofie Spjuth Max-Planck-Institut für Sonnensystemforschung.

Slides:



Advertisements
Similar presentations
Cylindrical and Spherical Coordinates
Advertisements

Earth Rotation The Earth spins slowly, making a full turn with respect to the Sun every day. We use the term rotation to describe this motion. The Earth's.
Earth.
Celestial Sphere Stars seem to be on the inner surface of a sphere surrounding the Earth.
Problem Solving For Conservation of Momentum problems: 1.BEFORE and AFTER 2.Do X and Y Separately.
The Earth Rotates.
OBSERVING THE SKY Chapter 1 Chapter 3 Constellations and Navigation Constellations and Navigation ORIGINS OF ASTRONOMY.
Newton and Kepler. Newton’s Law of Gravitation The Law of Gravity Isaac Newton deduced that two particles of masses m 1 and m 2, separated by a distance.
Section 1: Finding Locations on EarthFinding Locations on Earth
Locating Points on a Circle Sine Cosine Tangent. Coordinates Systems Review There are 3 types of coordinate systems which we will use: Absolute Incremental.
AST 112 Motion of Objects in the Sky. The Celestial Sphere Imagine you’re where Earth is, but there’s no Earth. What do you see? Keep in mind: – Nearest.
Mark Beckman - Flight DynamicsMB-1 Lunar Flight Dynamics Mark Beckman July 12, 2012.
Acute angle An angle with a measure less than 90 degrees.
Coordinate Systems.
Chapter 3 – Models of the Earth
Chapter 1 Predicting the Motions of the Stars, Sun, and Moon.
THE VIEW FROM EARTH. EARTH IN MOTION 1.Rotation: Period = 24 Hours 2. Revolution: Period = Days 3. Precession: Period  26, 000 years 4. Motion.
Earth-Moon-Sun Cycles. Cycle # 1 Day and Night Day  Night  Day  Night.
Chapter: The Sun-Earth-Moon System Table of Contents Section 3: Exploring Earth’s MoonExploring Earth’s Moon Section 1: Earth Section 2: The Moon—Earth’s.
Planet Earth A Grand Oasis in the vastness of Space
Motions of the Earth Ch Rotation the turning, or spinning, of a body on its axis. Two measurements for rotation Mean solar day is the time interval.
Bellringer EXPLAIN IN COMPLETE SENTENCES WHAT IS THE SYSTEM MOON - EARTH.
Models of the Earth Section 1 Preview Key Ideas Latitude Longitude Comparing Latitude and Longitude Great Circles Finding Direction Section 1: Finding.
Earth’s Size and Shape Measuring the Earth.
The Reason for the Seasons
Where in the world are we? … A system for describing location on the earth What is the shape of the earth … and how earth’s shape affects the process of.
Measuring Earth Midterm Review Topics: Earth’s true shape & evidence Positions on Earth (Latitude, Longitude, Angle of Polaris) Time Zones.
Table of Contents Title: Chapter 2 - Mapping our World –Page #: 17 –Date: 9/19/2012.
Sphere A round solid figure whose surface is at all points equally distant from the center.
MOTIONS OF SKY. Goals To identify the different parts of the celestial sphere model To understand how to express the location of objects in the sky To.
Chapter 20 Magnetism Conceptual Quiz 20 Conceptual Quiz Questions.
Aristotle, a Greek astronomer and philosopher who lived around 350 B.C., suspected that Earth was spherical. He observed that Earth cast a curved shadow.
OSIRIS Mars flyby : 3D reconstruction of Phobos and Deimos
Chapter: The Sun-Earth-Moon System
Earth Earth has a magnetic field Earth’s shape is a sphere which
Determination of photometric properties of Steins
Max-Planck-Institut für Sonnensystemforschung
Chapter 3 Objectives Distinguish between latitude and longitude.
Solar Energy and a Spherical Earth Chapter 14.1
Asteroid 4 Vesta observed from OSIRIS-ROSETTA
A TARGET OF THE ROSETTA MISSION
Deeper insight in the Steins flyby geometry:
11 Vectors and the Geometry of Space
Lutetia geometry and timeline
Summary of the science planned per mission phase
Vectors and the Geometry
1.5. Describing the Position of Objects in Space
Thermal modeling of rocky bodies
VIRTIS Operations at Lutetia
Properties of Earth— Spherical Shape 1
Copyright © Cengage Learning. All rights reserved.
Earth’s Rotation and Revolution
ASTRONOMY The Sun-Earth-Moon System
AIM: The Earth Sun System
Astronomy-Part 10 Notes The Earth-Moon-Sun Systems
Chapter 8: The Unit Circle and the Functions of Trigonometry
Vectors and the Geometry
CHAPTER 8 TIME AND TIME-RELATED PARAMETERS
Seasonal Change The seasonal change on the Earth occurs due to the tilt of Earth’s axis of rotation relative to the ecliptic, which is the plane of the.
BASIC ORBIT MECHANICS.
CHAPTER 8 TIME AND TIME-RELATED PARAMETERS
CHAPTER 8 TIME AND TIME-RELATED PARAMETERS
Earth and Moon.
11 Vectors and the Geometry of Space
Finding celestial objects in our night sky … … requires knowing celestial coordinates, based on the time of night, and our location Every star, cluster,
Chapter 8: The Unit Circle and the Functions of Trigonometry
Definition A Polar Coordinate System is a method of locating a point (r, ) in a plane where r is a distance from a point called the pole directed at.
LATITUDES AND LONGITUDES
Conceptual MC Questions
LATITUDES AND LONGITUDES
Presentation transcript:

Investigation of different flyby geometries for asteroid Steins - Surface area, stereo and phase angle coverage Sofie Spjuth Max-Planck-Institut für Sonnensystemforschung Katlenburg-Lindau, Germany OSIRIS Team Meeting , November 7, 2006

Reference system/Steins‘ system Opposite rotation Along rotation Z-axis – spin axis X-axis towards the Sun’s projection onto Steins’ equatorial plane Y-axis completes the right handed system Latitude Sun: φ The geometry of the flyby is equivalent to a fixed Steins and Rosetta approaching on a straight line with a constant relative velocity.

Assumptions/Constants/Constraints Steins is a sphere with radius 2.3 km Images taken at distances less than 100 000 km Two solutions of the rotation axis: 1. β = 265° ± 10°, λ = 8° ± 10° 2. β = 82° ± 10°, λ = 38° ± 10° Rotational period: 6.06 hours Constant relative velocity of 8.6 km/s Minimum distance of 800 km without a problem with the slew angle Cameras points towards Steins‘ center Solar elongation: 24° NAC (< 2h) 45° WAC

Inputs Separation angle & min resolution for stereo coverage Pole solution Trajectory direction Minimum distance Interval between images

Outputs Examples Area fraction coverege (of total surface) 0.7 Stereo fraction coverage (of total surface) 0.5 Images resolution range (km/pixel) 0.02 – 2.00 Phase angle coverage 0° – 150° Longitude/Latitude range

Area calculation Steins‘ divided into a grid with optional spacing in longitude and latitude Copied from: http://mitgcm.org/cubedsphere/latlongrid.html Retrieve the part that is illuminated by the Sun

The total area  sum of the imaged, illuminated pieces Longitude/Latitude matrix & Area matrix The total area  sum of the imaged, illuminated pieces Area of first image

Stereo area calculation Separation angle 5° Copied from: http://mitgcm.org/cubedsphere/latlongrid.html Resolution > 0.2 km/pixel

FLYBY‘s (view from above). 800 800 100 800 Flyby‘s in a plane with the Sun and Steins 1776 Flyby „above“ Steins

β = 265°, λ = 8° Dir. Min obs A frac < 200 m/pix S frac Phase angle coverage at closest approach A 800 0.629 0.510 0.505 0° - 150° 61° O 0.639 0.470 0.426 29° - 156° 119° 1776 0.645 0.506 0.502 0° - 140° 62° 528 0.508 0.503 18° - 151° - Sun’s latitude: -72°

0° phase angle occurs 3 minutes before closest approach at a distance of 1748 km. Closest approach Min phase angle

Longitude coverage: 357° Latitude coverage: 108° Steins

Area fraction of total surface: 0.629 Area fraction of total surface, res. < 0.2 km/pixel: 0.510 Stereo fraction of total surface, res. < 0.2 km/pixel: 0.505

β = 82°, λ = 38° Dir. Min obs A frac < 200 m/pix S frac Phase angle coverage at closest approach A 800 0.757 0.501 0.497 0° - 150° 61° O 0.797 0.468 0.440 29° - 156° 119° 1776 0.785 0.505 0.500 0° - 140° 62° 528 0.756 0.495 0.491 18° - 151° - Sun’s latitude: 53°

Flyby „above“ Steins A 800 0.629 0.474 0.467 28° - 151° 87° A 800 Flyby plane being offset relative to the Sun-Steins line by 800 km Dir. Min obs A frac < 200 m/pix S frac Phase angle coverage at closest approach A 800 0.629 0.474 0.467 28° - 151° 87° Compare with the trajectory in the Sun-Steins plane A 800 0.629 0.510 0.505 0° - 150° 61° Sun’s latitude: -72°

Pole solutions with error bars β λ A frac < 200 S frac Sun Lat. 265° ± 10° 8° ± 10° 0.54 – 0.72 ~ 0.50 -58° – -85° 82° ± 10° 38° ± 10° 0.68 – 0.83 41° – 65°

Conclusions Total area coverage between 54-83 %, depending on pole solution (amount of polar night region) Small differences of area fraction between cases of the same pole solution. But... - The 100 km flyby has problem with the slew constraint, thus the zero phase angle and closest approach is lost. - Trajectory opposite rotation (on the „back side“) performed at high phase angles - The original flyby (1776 km) return less images at low resolution than a closer flyby - Flyby „above“ Steins return no lower phase angles and have problem wtih solar panels rotation and illumination - Thus, the closest trajectory possible, without suffering from the slew constraint, along rotation and in a plane with the Sun and Steins, is the optimal flyby for area coverage and phase angle coverage