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THEMIS Extended Phase

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Remotely sense surface properties of lunar regolith. Result: ... reveal regolith surface properties. Secondary electrons. measured by Lunar ... – PowerPoint PPT presentation

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Title: THEMIS Extended Phase


1
ARTEMIS Lunar Exploration
THEMIS Extended Phase THEMIS baseline
ARTEMIS
2
Overview
  • THEMIS prime (FY08, FY09)
  • Overview, orbits, examples of data and
    discoveries
  • THEMIS Extended Phase (FY10, FY11, FY12)
  • Extended THEMIS Baseline (3 probes) ARTEMIS (2
    probes)
  • Acceleration Reconnection, Turbulence and
    Electrodynamics of the Moons Interaction with
    the Sun
  • The magnetosphere
  • The solar wind
  • The lunar wake
  • ARTEMIS for Planetary
  • Exospheric Composition, Sputtering Rates
  • Crustal fields wake deformation
  • Lunar interior sounding
  • Summary

3
TIME HISTORY OF EVENTS AND MACROSCALE
INTERACTIONS DURING SUBSTORMS (THEMIS)
  • PRIME MISSION (FY08 - FY09) SCIENCE GOALS
  • Primary
  • How do substorms operate?
  • One of the oldest and most important questions
    in Geophysics
  • A turning point in our understanding of the
    dynamic magnetosphere
  • First bonus science
  • What accelerates storm-time killer electrons?
  • A significant contribution to space weather
    science
  • Second bonus science
  • What controls efficiency of solar wind
    magnetosphere coupling?
  • Provides global context of Solar Wind
    Magnetosphere interaction

RESOLVING THE PHYSICS OF ONSET AND EVOLUTION OF
SUBSTORMS
FIVE PROBES LINE UP TO TIME ONSET AND TRACK
ENERGY FLOW IN THE TAIL
4
Mission overview Constellation in excellent
health
D2925-10 _at_ CCAS
Release
Probe instruments ESA ElectroStatic
Analyzer(coIs Carlson and McFadden)SST Solid
State Telescopes (coI Larson)FGM FluxGate
Magnetometer(coIs Glassmeier, Auster
Baumjohann)SCM SearchCoil Magnetometer (coI
Roux) EFI Electric Field Instrument (coI
Bonnell)
5
Prime mission orbits (FY07-FY09)
First 10 months(Feb 2007-Dec 2007)
First year baseline orbit (FY08)
2007-03-23
Tail 12008-02-02
2007-06-03
YGSE
Dayside 12008-08-08
Launch2007-02-17
2007-07-15
XGSE
Second year baseline orbit (FY09)
2007-08-30
2007-12-04
Tail 22009-02-18
Dayside 22009-09-16
6
First dissection of a detached FTE
Discoveries
Birth of storm-time ring current
Sibeck et al.,GRL, in press
Wang et al.,GRL, in press
Liu et al.,GRL, in press
First detection of remote signatures of
FTE's Dayside Traveling Compression Regions
7
New results (1st tail season)
Substorm trigger identified
Angelopoulos et al. submitted to Science
(embargo in effect)
8
THEMIS Extension (FY10,11,12)
9
ARTEMIS (P1,P2) FY10,11,12
FY10 Translunar injection FY11-12 6mo Lissajous
17 mo Lunar
10
ARTEMIS (P1,P2)
  • In the Magnetosphere, study
  • Particle acceleration X-line or O-line?
  • Reconnection 3D character and global effects
  • Turbulence Drivers and effects
  • Result
  • Reveal 3D distant tail, dynamics
  • In conjunction with
  • Solar wind monitors
  • ACE, WIND, STEREO
  • Inner magnetosphere monitors
  • Cluster, Geotail, FAST
  • Using the first
  • Two point dX, dY measurements
  • at scales from ion gyroradius to several RE

11
ARTEMIS (P1,P2)
  • Using first of a kind
  • two point measurementsat scales 1-10 RE, ideal
    for study of particle evolution in shocks, at
    foreshock and inertial range of turbulence
  • In the Solar Wind, study
  • Particle acceleration at shocks
  • Nature and extent of elusive low-shear
    reconnection
  • Properties of inertial range of turbulence
  • Result
  • Advance our understanding of particle
    acceleration and turbulence in Heliosphere
  • In conjunction with
  • Other solar wind monitors
  • ACE, WIND, STEREO
  • ARTEMIS is
  • High-fidelity solar wind monitor
  • In beacon mode if requested

12
ARTEMIS (P1,P2)
  • At the Moon/Wake
  • Study 3D structure and evolution of wake
  • Result
  • Advance our understanding of wakes at planetary
    moons, plasma void refilling around large objects
    (Shuttle, ISS, Hubble).
  • to better separate lunar surface and
    interiorsignatures in the context of
    environmental influences
  • Using first of a kind
  • two point measurementsat scales 0.1-10 RE,
    ideal for two-point correlations within wake and
    between wake and solar wind

13
ARTEMIS and Lunar Exosphere
ARTEMIS mass spectrometryof pickup ions plotted
as protons
  • Lunar Exosphere
  • Study composition, distribution of exospheric
    ions
  • Under a variety of solar wind conditions
  • Comprehensive instrumentation, ample statistics
  • Result
  • Advance our understanding of lunarexosphere and
    its variability
  • Goes beyond WIND observations

V?,y
H
V?,x
He
H2O
S
Solar Wind
ARTEMIS-2
Exospheric Pickup Ion
ARTEMIS-1
Hartle et al., 2005
14
ARTEMIS and Lunar Surface
  • Lunar Surface
  • Study composition and distribution of sputtered
    ions
  • Understand crustal magnetic fields, surface
    charging
  • Remotely sense surface properties of lunar
    regolith
  • Result
  • Advance our understanding of fundamental plasma
    interactions with planetary surfaces - with
    applications to Mercury, moons of Jupiter and
    Saturn, Pluto, KBOs, asteroids, etc.
  • Using first of kind
  • two point measurementsof ions and electrons
    near the Moon, with unprecedented energy coverage
    and resolution beyond LP electron reflectometry
    capability

Secondary electrons measured by Lunar Prospector
Halekas et al. 2008
Trace sputtered ions back to lunar surface
ARTEMIS
Secondary and photo-electrons accelerated from
charged lunar surface reveal regolith surface
properties
15
ARTEMIS and Lunar Interior
  • Unanswered questions about the lunar interior
  • Did the Moon form from a collision of Earth and a
    Mars size object?
  • How much of the moon formed from Earth and how
    from the impactor?
  • How deep was the lunar magma ocean? Does the Moon
    have a core?
  • Previous induction studies (Apollo, LP) support
    the lunar magma ocean hypothesis but are
    ambiguous due of low signal/noise ratio
  • ARTEMISs unique two point measurements allow us
    to separate external (inducing) and internal
    (induction response) fields at a wide range of
    frequencies, with much higher signal/noise ratio
  • Waves of T0.1-1hr provide information on crust
    and upper mantle
  • Waves of T1-5 hrs provide information on core
    (size, conductivity)
  • Study response to lobe perturbations shocks and
    North-South crossings

P1
P2
Core?
16
ARTEMIS and Planetary
  • In support of LRO
  • ARTEMIS provide comprehensive monitoring of Lunar
    Space Environment
  • Complements LRO/CRATER measurements below 200keV
  • Supports LADEE and NASs Scientific Content of
    Exploration of the Moon to
  • Understand the lunar atmosphere

17
Summary
  • THEMIS has delivered on its promises
  • Major discoveries from coast phase in GRL, JGR,
    SSR special issues
  • THEMISARTEMIS Continue to fully embrace
    community
  • All Data/Code Open Help line THEMIS_Software_Sup
    port Mirror sites proliferating in US, Europe
  • ARTEMIS Important for Heliophysics
  • ARTEMIS a new mission with very high science
    value per dollar
  • In novel orbits, with comprehensive
    instrumentation
  • Has tremendous potential to conduct key
    Heliophysics science from the moon
  • Addresses important Planetary questions of the
    moon
  • Supports major Lunar program missions (LRO, LADEE)
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