Title: THEMIS%20Extended%20Phase
1THEMIS Extended Phase Summary of THEMIS team
discussions (Please note this is work in
progress)
2Preamble
- P3,4,5 will be uniquely suited to study
microphysics at small scale separations - Equatorial magnetosphere at 9-12 RE was not
studied by Cluster - Having explored Rf, fq planes during prime
mission, THEMIS ready to explore 3rd dimension
Rq - Rq plane is optimal three-probe configuration for
studying currents in the tail and at the
magnetopause - Tail Region 9-12RE is unique to substorms
- Auroras and substorm onset currents map there
- Region is important for MI coupling during
substorms and storms - Dayside Region 9-12RE is unique to Solar Wind
Magnetosphere coupling - Sub-solar Magnetopause streamlines affect energy
entry along entire magnetopause boundary - Reconnection topology and rate have not been
studied before due to lack of multi-point
observations - Exciting new possibilities with THEMIS P3,4,5 at
10-100km separations at those regions - Prepares the ground for MMS-like studies
- Early dayside period on THEMIS (coast phase)
provides a glimpse of capabilities - Early dayside period shows operational complexity
of achieving small scale separations - P1 will be unable to contribute to the above
goals due to extreme shadows - Inclination changes dont help because apo-apsis
is at the equator/ecliptic intersection - Apogee lowering is costly and cumulative
precession post-prime mission does reduce shadows - Anticipated since CDR but could not afford
time/cost to verify or fix by design changes - P2 may be able to contribute uniquely to inner
magnetosphere science
3P1, P2 shadows, nominal orbits
Representative shadow trends for typical P1
orbits (from THEMIS CSR). Note underestimates
3rd year shadows exceed design limit 180min
RAP330deg
4P1 180/360 Minute Eclipse Power
- Battery Capacity 11.8 Ah
- Battery Depth of Dishcarge (DoD) Requirement lt
65 - 3hr Eclipse DoD 63
- Margin 2
- Battery Average Voltage 28.8V
- Battery Capacity 340 Wh
- Eclipse Power Reqs 69.5W
- Max Eclipse Sustainable 4.8h
- No recovery for BAU if battery is drained and BAU
stops operating
5Thermal Design and Test Limits
Qual Limits
Operational Limits
Predicts
Minimum Predicted
5C
5C
Maximum Predicted
5C
5C
10C
10C
-100C
-120C
-110C
- Bus Thermal Design goal was to be at least 5 C
inside Operational Limits for passive design
components. For side panels, Qual limit was
120C - FM-1 (TH-A, P5) Qual-tested at 10C beyond
Operational Limits - FM 2-5 Acceptance tested at 5C beyond
Operational Limits
6P1 180 minute Eclipse Temperatures
A 15deg difference between Localand Bulk Side
Panel temperatures Cold spots on the arrays
wouldresult in break of the vaultedinterconnects
and the cell glass LOSS OF PRIME POWER
7P1 180/360 Minute Eclipse Transient Temperature
Results
-95oC
Side Panel local temperatures may exceed
operational cold limits (-95o 15o -110oC)
8P1, P2 can they be saved at Earth orbit?
- P1 consuming all 300m/s (remaining at end of
mission) in Earth orbit, options - Apogee reduction to 18RE on Oct 1, 2009 (300m/s)
Exacerbates P1 shadows Not an option - Inclination change in June 2009 (change in 2nd
dayside season) may reduce shadows (TBD) - 40deg inclination change slows down APER changes,
may go through minimum shadow in 2010 - In 2011 the long shadow will be inevitable
- Basic reason line of apsides is at the
equator/ecliptic intersection - No de-orbit fuel left (128m/s are required) -
Does not meet de-orbit requirements Not an
option - Summary P1 cannot be salvaged with remaining
fuel in Earth orbit - Would have to deplete all fuel and placed on a
re-entry path - If it survives shadows, Lunar perturbations will
render orbit polar. Even less useful for P2-5
then. - P2 consuming 450m/s (remaining at end of
mission) in Earth orbit, options - Additional inclination change and perigee change
may reduce shadows further - Requires further investigation
- Depends on fuel margin consumed in prime mission
- At same altitude not so helpful for extended
science with P3,4,5 - Apogee reduction to 12RE on Oct 1, 2009 (210m/s)
builds 5deg additional precession - Can be brought closer to P3,4,5
- Can be used to validate current sheet orientation
assumption - Summary P2 can be salvaged with its remaining
fuel in Earth orbitbut scientific usefulness
and orbit optimization require further study
9P3,4,5 tail science P1P2 relationScience of
P1,P2 at current orbits peripheral
- Focus at 10-12RE post prime-THEMIS
- Most important unresolved substorm questions
- Magnetosphere-ionosphere coupling at onset
- How are tail currents diverted to ionosphere?
- How are plasma sheet particles accelerated?
- How do quasi-static electric fields build up?
- Micro-physics of onset mechanism
- If at CD site, extended THEMIS can address
- If at Rx site, MMS will do that in the future
- 1st extended year
- Take P5 to P3,4 altitude (Dec 1, 2009), dV60m/s
- Separate P3-P4 in radial direction (both
siderial) - Study 0.1 1RE scale sizes currents, flows, CD
- 2nd , 3rd extended year
- Take P5, P3 closer to P4 (Dec 1, 2010)
- APER180, P5 d(inc) 6deg, dV 110m/s
- Tune period and phase to optimize geometry
- Study 10km-1000km scale sizes
- By the 1st year of THEMIS extension
THEMIS April 15-19, 2010 w/o maneuvers
P1
P2
P4
P5
P3
10P3,4,5 tail science
- Focus at 10-12RE post prime-THEMIS
- Most important unresolved substorm questions
- Magnetosphere-ionosphere coupling at onset
- How are tail currents diverted to ionosphere?
- How are plasma sheet particles accelerated?
- How do quasi-static electric fields build up?
- Micro-physics of onset mechanism
- If at CD site, extended THEMIS can address
- If at Rx site, MMS will do that in the future
11P3,4,5 tail science P1P2 relationScience of
P1,P2 at current orbits peripheral
- Consensus
- Use P3,4,5 for Cluster-like science
- Study equatorial magnetosphere
- Cluster did not visit 10-12RE plasma sheet
- Optimize orbits to do cutting edge research
- In different configuration than before
- Send P2 to join P3-5?
- Determine whether or not fuel permits P2 to join
P3-5 in a tetrahedral formation - Finalize decision no earlier than 10/2008
- Send P2 to join P1 in ARTEMIS at moon?
- Determine whether ARTEMIS needs one or two THEMIS
S/C (in view of pending LuSIE and LEO
selections) - Finalize decision no later than 03/2009
12P3,4,5 tail science T3 (2010-04-15)
T3, GSE coords View from tail along
NS dZ(P3-P5) 600-3000km dR(P3-P4)1RE gt
dZ every 8 days
Y
P3
P4
P5
13P3,4,5 tail science T3 (2010-04-15)
Z
Y
P3
P4
X
P5
T3, GSE coords View from dawn along
NS dZ(P3-P5) 600-3000km dR(P3-P4)1RE gt
dZ every 8 days
14P3,4,5 dayside science D3 (2010-11-01)
D3, GSE coords View from Sun along
Ecliptic dZ(P3-P5) 1000-3000km dR(P3-P4)1000km
lt dZ every day Apogee12Re
Z
P5
Y
P4
P3
X
15P3,4,5 dayside science D3 (2010-11-01)
Z
P 5
P4
P3
X
Y
D3, GSE coords View from dawn along
Ecliptic dZ(P3-P5) 1000-3000km dR(P3-P4)1000km
lt dZ every day Apogee12Re
16P3,4,5 tail science T4 (2011-05-10)
Z
Y
T4, GSE coords View from dawn along
NS dZ(P3-P5) 100-500km dR(P3-P4)1000km gt
dZ every day Apogee 12RE
X
17P3,4,5 science during last year FY12
P3,4,5 dayside science D4 (2011-12-01) Same
configuration as D3, except smaller
separations dZ (P3-P5) 200-1000km dR
(P4-P3/P5) 200km P3,4,5 dayside science T5
(2012-06-21) Same configuration as T4, except
except smaller separations dZ (P3-P5)
200-1000km dR (P4-P3/P5) 1000km
18Summary P3,4,5 science at 10-12RE Cluster-class
science at an uncharted region
- Key science questions in the tail at 10-12RE
region - How does the cross-tail current get disrupted at
substorm onset? - If current disruption is responsible for
substorm onset, what is the plasma physical
process? - If reconnection causes current disruption, how
does incoming flow disrupt the cross tail
currents? - Which are the cross-tail current carriers and
how does their free energy get reduced? - How does the cross-tail current get diverted
into auroral ionosphere at onset? - By vorticity generation, by pressure gradient
redistribution, by flow breaking or by Alfven
waves? - THEMISs unique Rq configuration provides
unprecedented measurements in this region of
space. With Cluster-quality instrumentation and
orbital separations, in a region never before
visited in such a formation, THEMIS will measure
cross-tail and field aligned current
measurements, particle distributions, and waves
will be able to answer which mechanism is
responsible for the current disruption and
diversion at substorm onset. - Key science questions in the dayside at 10-12RE
region - How solar wind energy couple through the
subsolar magnetopause? - Do cold ions in the equatorial magnetosphere
affect reconnection rate and energy coupling? - What is the extent, topology and rate of
reconnection at the subsolar magnetopause? - THEMISs unique Rq configuration provides
unprecedented reconnection inflow measurements
from P4, with simultaneous bracketing of the
diffusion region by P3 and P5. With
Cluster-quality instrumentation and orbital
separations, THEMISs three satellites measure
(assuming azimuthal invariance) magnetopause and
field aligned currents for the first time in this
critical region.
19How can P2 help P3,4,5? Ans. If it creates good
tetrahedron
- P2 can be brought to siderial orbit
- Daily conjunctions with P3,4,5
- Optimized separations to 1RE
- Provides additional CD timing/context
- Validates 2D planar current sheet
- P2 can be further tuned
- Tetrahedral formation with P3,4,5
- Requires MMS/Cluster know-how
- Study initiated (Concha/Hapgood)
- P2 may require inordinate fuel
- Significant science return
- Cluster was never there
- MMS will not have 0.1-1RE scale
- Summary P2 may be able to dosignificant
additional science ifplaced at tetrahedral
formationwith P3,4,5 but it is unclear at this
point if fuel margin is sufficient for orbit
maintenance.
Y
2010-04-10 000000
P2
P4
X
P3
P5
20Optimal use of P1, P2 ARTEMIS
- P1, P2 have sufficient fuel to raise apogee to
the moon - Easier to go up than down
- Lunar gravity perturbs orbits sufficiently to
remove long shadows - Probes need not stay any longer in Earth orbit
- Mission design and operations can become complex
and expensive unless new target is found - Use the moon as anchor to perform new tail and
new Solar Wind science - Permits exploration of a unique Lunar-Solar and
Lunar-Tail environment like never done before - Optimal use of de-orbit fuel (lunar re-entry)
- Design considerations for Lunar insertion, result
in a robust mission - Spin axis at ecliptic normal throughout mission
optimal communications - Equatorial Lunar orbit stable for many years
- After Lunar Orbit Insertion operations are
routine - A 24hr orbit guarantees
- Less than 3.5hr shadows, acceptable for probe
design - Familiar, low risk power, thermal and operations
environment - Mission design that satisfies above criteria is
robust - Under study by JPL since April 2005
- By same team which validated the THEMIS mission
design in 2004-2005 - JPL review on 2007-Nov-02 found no technical
issues
21ARTEMIS Acceleration, Reconnection, Turbulence
and Electrodynamics of the Moons Interaction
with the Sun
22What are the important magnetosphericquestions
after THEMIS, before MMS?
Distant magnetotail (after Geotail and WIND
single spacecraft) What is the nature and extent
of the distant tail neutral line? Does the tail
vanish in response to Interplanetary Coronal Mass
Ejections? What are the dimensions and topology
of plasmoids (carry ½ energy of storms) Answers
necessitate multiple THEMIS-type satellites at
0.1-10RE scales Solar Wind and Shocks (after
multiple missions Cluster, ISEE1/2) How do
shocks accelerate particles? (Shock acceleration
or diffusion) What is the nature of solar wind
turbulence in 1-10RE scale lengths (no data)
Answers necessitate multiple THEMIS-type
satellites at 1-20RE scales Lunar Wake (after
Lunar Prospector and WIND) What are the plasma
waves that make up the nature of the Lunar
Wake? How does the wake fill-in from near the
moon to far down What makes up, sustains and
dissipates the electric fields behind the wake
Answers necessitate multiple THEMIS-type
satellites at 1000-50,000km scales
23ARTEMIS Science Objectives
- Acceleration in shocks, tail and lunar
environment - What is the nature of acceleration at shocks?
- Follow evolution of particle distributions at
two points along the shock. - How do MeV electrons get accelerated in the
tail? - Measure field topology, particle spectra and
evolution in time and space. - How do energetic (100s of keV) ions and
electrons get accelerated in the wake? - Measure particles and fields in the wake and the
solar wind simultaneously. - Reconnection
- What is the distant tail reconnection onset
mechanism, effects and response to solar wind
drivers? - Spontaneous or induced?
- Continuous or impulsive?
- Answers necessitate multiple THEMIS-type
satellites at 1-20RE scales - Lunar Wake (after Lunar Prospector and WIND)
- What are the plasma waves that make up the
nature of the Lunar Wake? - How does the wake fill-in from near the moon to
far down - What makes up, sustains and dissipates the
electric fields behind the wake - Measure particles and fiels in the wake and
outside at 1000-50,000km distance
24ARTEMIS Mission Profile
25ARTEMIS Mission Phases
Phase I (Oct 09 Oct 10) - placement
26ARTEMIS Select Orbits
Phase II (Oct 10 Jan 11) Opposite Sides
Sun-Earth Alignments
27ARTEMIS Select Orbits
Phase II (Oct 10 Jan 11) Opposite Sides
Dawn-Dusk Alignments
28ARTEMIS Select Orbits
Phase III (Jan 11 Apr 12) Same Side
Sun-Earth Alignments
29ARTEMIS Select Orbits
Phase III (Jan 11 Apr 12) Same Side
Dawn-Dusk Alignments
30ARTEMIS Wake Crossings Phase II,III
31ARTEMIS Wake Crossings Phase II,III
32ARTEMIS Distant Wake CrossingsA Perspective
dB
33Phase IV (Apr 12 May 13) ARTEMIS After
Insertion
34ARTEMIS Wake Crossings
35ARTEMIS Ground Operations Concept
- Alternate Downlink OVRO
- RefurbishmentOps 1M
- Can track gt3hrs/day
- A 40m dish better than DSN
- Saves government gt10M
OVRO, 40m TLM Receive Only
DSN, 34m TLM, TRK, CMDTranslunar Orbits
BGS, 11m TRK CMDLunar Orbits
- Flight Dynamics
- Translunar Orbit
- JPL Mission Design, Orbit Determination,
Ephemeris, Maneuver Planning - UCB Attitude Determination
- Lunar Orbit
- UCB Mission Design, Orbit/Attitude
Determination, Ephemeris, Maneuver Planning - Mission Operations (UCB)
- Pass Scheduling, Mission Planning Command
Generation - Data Trending Anomaly Resolution, ITOS CMD
Control - Science Operations (UCB)
- Follows Standard THEMIS practices
36ARTEMIS Science Team
Tail Plasmoids, Scales Slavin, Murphy
Rx/Heating Oieroset, Schriver
Turbulence Weygand, Velli
Acceleration, Scales Slavin, Murphy
Solar Wind Shock acceleration Eastwood, Bale
Turbulence Velli, Weygand
Foreshock Eastwood
Wake Computer sims Travnicek, Schriver, Farrell
Laboratory sims Gekelman
Exosphere Delory
Refilling, Beams Halekas, Farrell, Bale
37THEMIS Extended Phase Proposal
- Senior Review panel
- Decides how to apportion funds between
continuing missions (Voyager, Cluster ) - Evaluates and approves plans for FY09/10 hears
proposals for FY11/12 - THEMIS ends in FY09, would request funding for
FY10 and present plan for FY11/12 - THEMIS extension funding request for FY10 with
further extension in FY11/12 - ARTEMIS proposal to slowly ramp up in FY08/09
and move to operations in FY11/12 - Costs
- Cost Guidance would be sufficient to continue
THEMIS with minimal operations - Hinges on scientific publications and
discoveries made by THEMIS now - Reviewed on basis of past performance as
indicator for future output - Guest Investigator program to accompany THEMIS
extended mission, also possible - Hinges on quality and accessibility of THEMIS
data, and community involvement - Cost increase due to ARTEMIS team and mission
operations may necessitate new funds - Senior review panel chair may have to obtain
additional funding from Heliophysics director - Received recommendation to proceed with a
combined proposal - Timeline
- Proposal due February 21
- Review of Mission Archive Plan March 2008.
Presentations April 8-11. Selection Jun 12,
2008