ostst, hobart, march 2007 - 1- future altimeter systems : is mesoscale observability guaranteed for...
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OSTST, Hobart, March 2007- 1-
Future altimeter systems : is mesoscale observability guaranteed for operational oceanography?
Future altimeter systems : is mesoscale observability guaranteed
for operational oceanography?
P.Escudier, G.Dibarboure, J.Dorandeu, CLS, Space Oceanography Division
OSTST, Hobart, March 2007- 2-
Future altimeter systems : is mesoscale observability guaranteed for operational oceanography?
Overview
• Until recently, the exceptional longevity of T/P and GFO added to the performance of Jason and ENVISAT were hiding the risk of future data gaps.
– The current missions are still performing well but exceeding designed lifetime
• With the current launch schedule (Jason2, CryoSat, AltiKa, Sentinel…) can we guarantee a sufficient mesoscale observability for new and developing applications and for operational oceanography ?
• Use a probabilistic model to better assess the odds of having an observing system (multiple altimeters) accurate enough :
1
GEOSATT/PERS
T/PERSGFO
JASONT/Ptandem
ENVISATGFO
JASONENVISAT
GFO
Oct1992
T/PT/PERS
2 3 4 3Jan
2000Oct
2002Sep2005
1 2Dec1993
Mar1995
Nov1986
Dec1988
?
JASON-2Cryosat2?Sentinel?GMES?AltiKa?
20082009
1234
Insufficient for offline meso-scale applications
Minimum for off-line applications
Robust for offline applications (barely for real time)
Robust sampling for real time applications
Color Legend
• Minimum needed to monitor mesoscale structures :
– 2 satellites in delayed time (offline),
– 3 satellites or more in near real time (Pascual et al)
Question asked in Venice meeting (2006)
OSTST, Hobart, March 2007- 3-
Future altimeter systems : is mesoscale observability guaranteed for operational oceanography?
EKE (cm²/s²)
J1 J1+E2
J1+E2+TP J1+E2+TP+G2
EKE on [october 2002 – june 2003]
+ 40% J1
+ 15% J1+E2
50 350
EKE in the Mediterranean sea depending on the satellite configuration
OSTST, Hobart, March 2007- 4-
Future altimeter systems : is mesoscale observability guaranteed for operational oceanography?
Approach and model used
• Lifespan probability model of a satellite driven by platform and payload design. – Probability function approximated with a simple model fitted on lifespan
computations from AAS
00.2
0.4
0.6
0.8
1
0 1 2 3 4 5 6 7 8 9 10 11 12
Launch (100% success rate assumed)
Lifespan (75% survival chance)
Mission should not outlive 2.2 * nominal lifespan
• Probability function for Each mission based– launch date, – expected lifespan as announced– specific cases taken into account
• Cryosat considered as 50% operational on ocean : payload limitation, non-repetitive ground track
• Lifetime limitation – ie propellant limit for ENVISAT
• Missions grouped by ground track :– redundant measurements are not
stacked, but likelihood to have the ground track covered increases
• Individual probability function combined to compute combinatorial probabilities Probability function used for an altimeter with a 5 year
lifespan
OSTST, Hobart, March 2007- 5-
Future altimeter systems : is mesoscale observability guaranteed for operational oceanography?
Model validation• The probability model is validated using historical datasets.
– actual coverage on ocean taken into account : platform/payload events, …
• Agreement between model prediction and observed reality fairly good
• Most significant differences :
– GFO post-launch anomalies
– unexpected longevity of T/P
• In both cases, the event is against the base probability assumptions on the satellite : 100% success rate at launch, and 2.2 * lifespan max
01
23
45
1992 1994 1996 1998 2000 2002 2004 2006
Unexpected post-launch anomalies on GFO
T/P and ERS still in operations (50% chance)
Exceptional longevity of T/P
(and GFO)
01
23
45
1992 1994 1996 1998 2000 2002 2004 2006
Unexpected post-launch anomalies on GFO
T/P and ERS still in operations (50% chance)
Exceptional longevity of T/P
(and GFO)
Model Reality
ERS1
ERS2
T/P
GFO
Jason1
ENVISAT
Data losses
Number of Altimeters in operation
OSTST, Hobart, March 2007- 6-
Future altimeter systems : is mesoscale observability guaranteed for operational oceanography?
Will altimetry provide the input needed by near real time applications ?
• Probability to have the minimum observing system needed to monitor mesoscale : – 2 satellites for delayed time applications (red), – 3 satellites for near real time applications (blue)
• Critical situations– Probability less than 10% in 2008
for near real time applications,Probability less than 25% until CryoSat.
– Odds fall down to 30% after the scheduled end of ENVISAT in 2010, and until both Sentinel-3 are operational
• Results are arguably optimistic:– altimeters assumed to be
operational just after launch – 100% launch success rate
• HY-2 to be added• Jason-3 to be confirmed• Launch dates to be tuned
according to latest infos 00.2
0.4
0.6
0.8
1
2007 2008 2009 2010 2011 2012 2013 2014
Jason-2 (old T/P track, not stacking
with Jason-1)
CryoSat
Jason-1 tandem phase (new ground track covered)
AltiKa
End of ENVISAT
Sentinel-3x 2
00.2
0.4
0.6
0.8
1
2007 2008 2009 2010 2011 2012 2013 2014
Jason-2 (old T/P track, not stacking
with Jason-1)
CryoSat
Jason-1 tandem phase (new ground track covered)
AltiKa
End of ENVISAT
Sentinel-3x 2
Jason -3
Probability to get 2 satellites availableProbability to get 3 satellites available
OSTST, Hobart, March 2007- 7-
Future altimeter systems : is mesoscale observability guaranteed for operational oceanography?
Jason tandem phase• The probabilistic model was used to explore alternate scenarios and to assess
the impact of various decisions on the minimum observability needed for Near Real Time applications and operational oceanography
• As an illustration, shifting Jason-1 on a different orbit (tandem phase, similar to the Jason/TP phase in 2003/2005) would improve the NRT odds by 20%
• The cross-calibration of both Jasons is mandatory, but if the tandem phase does not start six months after launch, the odds of getting the minimum NRT data reach 0%
00.2
0.4
0.6
0.8
1
2008 2009 2010 2011 2012
Tandem phase after 6 months ? 0% chance of minimum NRT coverage
Tandem phase after 6 months(up to 20% chance increaseto get the minimum NRTobservation)
00.2
0.4
0.6
0.8
1
2008 2009 2010 2011 2012
Tandem phase after 6 months ? 0% chance of minimum NRT coverage
Tandem phase after 6 months(up to 20% chance increaseto get the minimum NRTobservation)
Probability to have the minimum NRT observability without a Jason-1 tandem mission (green), or with a Jason-1 tandem phase 6 months (red) or 1 year (blue)
after the launch of Jason-2
OSTST, Hobart, March 2007- 8-
Future altimeter systems : is mesoscale observability guaranteed for operational oceanography?
Exploiting CryoSat data
• Similarly, an additional 20% chances can be gained if CryoSat data are fully exploited with a complete coverage on ocean (ice + ocean as primary mission), and better geophysical corrections/references :
– improved MSS to balance out the non-repetitive ground track,
– Improved model for ionosphere correction
– Improved model for wet troposphere correction
00.2
0.4
0.6
0.8
1
2009 2010 2011 2012 2013 2014
20% chance increase to get the minimum observation in NRT with perfect ocean coverage and optimized processingProbability to have the minimum NRT
observability with opportunistic ocean data from an ice-oriented CryoSat
(blue) and with perfect ocean coverage and improved geophysical corrections
(green)
OSTST, Hobart, March 2007- 9-
Future altimeter systems : is mesoscale observability guaranteed for operational oceanography?
Summary and Conclusions
• Minimum number of satellites in operations needed to monitor mesoscale structures :– 2 satellites in delayed time (offline studies)
– 3 satellites or more in near real time
• Simple probability model used to assess the odds of having an observing system (multiple altimeters) accurate enough to provide the input measurements needed for offline and Near Real Time applications
• Validation with historical data : good consistency and global predictions but unexpected boolean events (T/P longevity, launch failure…) Improvements possible on model
• Offline mesoscale observability is likely (P>60% after Jason-2)
• Odds of meeting the NRT requirements are very poor until Jason-3 + both Sentinel-3 (P<25% until 2010, and 40% until 2011). It is ironically when operational oceanography and NRT applications start to be fruitful that NRT altimeter data may be lacking.
• Odds can be improved with a Jason tandem phase or a better use of CryoSat on ocean
• One more reliable altimeter launched before 2013 would almost double the NRT odds