Title: Future altimetry design From impact studies to operational metrics or the reverse
1Future altimetry designFrom impact studies to
operational metrics or the reverse ?
G.DibarboureJ.DorandeuP.Escudier
2Introduction
- Should early impact studies define operational
metrics or the reverse ? - Framework support to future mission design
(ESA, CNES, Eumetsat, Ifremer) - Definition of Sentinel-3, Phasing options for the
Jason tandem - Figure of merits for future altimetry concepts
wide-swath, large constellations - Impact of payload changes noise level
reduction, cost reduction - Exploratory studies
- Iterative process (mission concept ? performance
assessement) - CLS Toolbox for Mission Analysis Testing and
Optimisation (TOMATO) - Two types of analysis mission analysis OI
based OSSEs - Need simple yet compelling results
- Subtle payload differences ? ? Metrics used must
give a clear answer - Conflicting mission objectives (e.g. OC vs
Altimetry on S3) ?? Altimetry metrics must be
convincing for decision-makers? E.g 15 of
additional variability observed is not convincing
for neophytes - Illustration of the DUACS approach through two
ongoing studies Post-EPS reference orbit
High-resolution altimetry
3Example 1 Post-EPS reference orbit
- Question asked by Eumetsat which orbit should
be used for future reference missions ? - Reference orbit (T/P, Jason) is exceedingly
aggressive - Onboard anomalies and failure (Jason-1 has burnt
most redundant safeties) - The motivations behind the TP orbit choice are no
longer major constraints - Many factors to take into account
- History and existing time series
- Sampling capability, Aliasing issues
- Error budget (e.g. POD performance vs orbit
parameters) - Many applications climate, mesoscale, ice
monitoring, hydrology - Mission cost (launch, operations, mission
lifespan) - And other altimetry missions !
- Unlikely to find a single perfect orbit, so the
study rationale is to - Sort out (many) bad options ? first filter no
time wasted - Analyze orbit candidates with more details ?
second filter process when in doubt, trash it - Keep only a handful of interesting orbits for the
community to check out
4Post-EPS Aliasing analyses
- First filter orbit geometry and base properties
- Acceptable altitude and inclination range
- Repetitive
- Acceptable repeat (sub)cycle duration
- Optimal to host a tandem of 2 altimeters
- Second filter tidal components
- Must allow tidal wave observation within 3 to 5
years(aliasing under control) - Tidal components must be separable within a
reasonable time span - Basic selection leads to 1400 options
- Drastic separability requirements 0 option
- Trade-offs ? many options with different
pros/cons
5Post EPS multi-satellite sampling analysis
- Geometrical sampling analysis (no model, no OI)
- Observation quality (correlation between
structure and observation) - Ability to detect mesoscale changes in NRT
- Observation isotropy (e.g. currents mapping,
crossovers) - Structure monitoring/tracking capability
-
- Protocol validation on historical missions
- After this screening process 12 candidates
interesting
6Post-EPS - Output of step 1 first orbit
selection
Initial selection (tidal filter nominal)
Additional selection (relaxed tidal aliasing
requirements, except on 4-9 cpy climate band)
7Post-EPS Mesoscale sampling capability (1/2)
- Analysis performed from OI OSSE based on Mercator
simulations - Mercator reality ? Observation simulated ? OI
used to reconstruct - Reconstruction error gives access the sampling
capability
8Post-EPS Mesoscale sampling capability (2/2)
- Once suboptimal options are removed, the mapping
processoffsets uneven sampling ?
minordifferences - Sampling error on U/V vary by 10 in non
coordinated tandems - Impact of orbit inclination on sampling isotropy
still still visible after mapping (especially
combined with high-inclination S3) - Three good candidates (T/P-like with 10 more
data thanks to lower altitude) results coherent
with geometrical analysis - SWOT orbit 22d is not the best option to host
(only) a traditional altimeter - Any contribution from GODAE would be useful to
complete this study (model-based OSSE, metrics
suggested)
9Example 2 High resolution altimetry
- Explore the benefits of a 24 satellite
constellation (Nadir only) - Next generation of Iridium altimeter payload
passengers ? - Cost minimized (minimal payload, error budget
tradeoffs) - Comparison to a global wide-swath altimeter
observation - Impact of noise reduction (AltiKa, doppler
altimetry, SWOT) - First step geometrical analysis
- To provide a first quantification of the benefits
- To tune the altimeter payload distribution on the
66 potential Iridium slots - To explore multiple timespatial scales (e.g.
meteo, mesoscale, submeso) - Second step OI impact study on (sub)mesoscale
- Needed to quantify the impact on currents and
vorticityand the HF or short scale specific
error - Work performed with support from CNES and Ifremer
Up Jason cycle / sub-cycle scanning
pattern Down Space/Time scale observation limit
10High-resolution altimetry geometrical analysis
Constellation detection and monitoring skill
(left 150km, right 20km)
Instantaneous correlation between one snapshot
and past altimetry data (realistic correlation
model 150km/15d, arbitrary snapshot from day 12)
11High-resolution altimetry OI impact study
Model EKE Los Alamos 1/10
- Reality used POP or Earth Simulator (ES)
outputs - Configurations analysed 1 to 4 sats, 24 Iridium,
SWOT - Realistic error levels on simulated observations
- Ongoing work
- Actual mapping reconstruction error (H,U/V,
Vorticity) - First step crude mapping parameters (100km, 5
to 10d) - Separation of error on HF/LF content (time
space) - Separation of error from mapping limitations
sampling limitations - For POP content SWOT sampling is good and Iridium
excellent - For ES, SWOT temporal sampling is more
problematic, but correlation scales must be
revisited
2000cm²/s²
Model EKE ES
12High-resolution altimetry impact of noise level
SSH power spectrum (Jason-2 simulated data from
ES reality variable HF error level)
- Starting question how does the altimeter data
high frequency error (instrument noise,
processing error) affect the power spectrum ? - Earth Simulator output ? Sampled along altimetry
ground tracks (50 days of ideal obs) - Variable white noise ? Realistic observations
- Consistent with spectrum slope of actual data in
GulfStream (-3.4 for 90-200 km for 2.5 to 3cm
HF content) - Impact of SWOT rollbaseline error far range
spectrum is K-3 and increasing to K-11/3 as the
data get closer to the Nadir position in swath - Reducing the high-frequency error is important
Ka-Band, Doppler, SLOOP project processing
3 cm
K-5 or K-11/3 ?
1 cm
3 mm
13Summary and Conclusion
- Overview of ongoing studies
- Long term questions new reference orbit, impact
of HF error, high-resolution sampling - Short answers 3 good orbits, reduce the noise,
attractive 24 satellite concept (complement to
SWOT ) - Two-types of studies carried out by CLS mission
analysis OI impact studies - Excellent way to explore unusual configurations
or numerous variants (sort out poor options) - Some metrics are more convincing for
decision-makers than classical resultsE.g.
mesocale can observed in real time with 12
satellites is a stronger message than 4
mesoscale observation error removed with 8 sats - Full science content must be consolidated
afterwards (finer quantification once the general
concept is nailed down) - Past impact studies helped define current
operational metrics (DUACS K.P.I) - Conversely any operational metric can be deployed
for such a demonstration - This logic is applicable to GODAE models
design/impact studies ? operational metrics - For future concepts, we need to be consistent
with future operational metrics - What routine-to-be metrics should be used to help
design future observing systems ? - So what will be requirements of GODAE models in
2018 ?