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The Road to RL05 Srinivas Bettadpur for the UTCSR GRACE Team.

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Presentation on theme: "The Road to RL05 Srinivas Bettadpur for the UTCSR GRACE Team."— Presentation transcript:

1 The Road to RL05 Srinivas Bettadpur for the UTCSR GRACE Team

2 Framework for Product Improvement What are limiting models? What can KBR data tell us? Methodology will be refined No changes planned to flight segment Obs a priori models - PredictProcess Estimate x + Interpret Product improvements are planned Changes made during the re- processing will affect interpretation

3 Summary Points Changes to parametrization will continue to reduce Level-2 product artifacts. We are exploring methods for improving the Level-1B data products. What does the data itself tell us about sub-monthly variability?

4 Methodology: For Example

5 RL04 300 km smoothing

6 Going in right direction… 300 km smoothing

7 Level-1 Product Improvement Previous experience suggests candidates for further improvement. KBR1B: –Removing high-frequency noise ACC1B: –Thermal corrections –Modeling of heater spikes and other artifacts? SCA1B: –In review… Other options remain to be explored.

8 What can the KBR data tell us? Analyze spatio-temporal distribution of KBR data to investigate reasons for residual sub-monthly variability of the data. Typical approaches: –Remove “best-fit” orbit from KBR data. –Some kind of low-pass filtering is necessary for noise reduction. –Frequently, numerical differentiation is used to enable assessments of range-acceleration data residuals. This Study: Looks at “pre-fit” residuals only –400 days studied from May 2006 through May 2007 –Two modeling standards used: RL04 RL04 + mean-field update + annual model of variability –POD with gps, acc, att and kbr data - in daily orbital arcs

9 KBR Fit Statistics Improved models reduce variance dominantly in the mid-frequency range. (Not shown): The daily raw KBR1B statistics are dominated by noise at 0.26 micron/sec levels in the high- frequency bands. –This must be removed for effective “regional” study of the data. Why is there such a large day-to-day variability in the RMS contributions from each frequency band?

10 A Note on the Mechanics “Glitches” will typically show up as large North-South patterns in the maps drawn from this data. –This study did not use the same level of rigorous editing used in making monthly solutions. User Resources: The project provides an SOE with complete details necessary to spot and avoid these problems.

11 Month-to-Month Variations Each panel shows the standard deviation of “pre-fit” accelerations within each 3° bin. “Blobs” are approx ±6 nanometer/sec^2 (full scale is 9 nm/s^2). “Blobs” in the same location wax and wane through the year. What is all this?

12 Close-up : July 2006

13 Attempted Fit to Tides (N2, M2 & S2) Tides appear to account for no more than ≈2 nm/s^2 signal rms over small regions. An observation from images not shown: Fitting monthly N2 & M2 harmonics does much better at variance reduction, and across more of the blobs.

14 The M2 Solution

15 The N2 Solution

16 The S2 Solution For the purpose of de-aliasing, it may be sufficient to devise a tidal correction model in the data-space (range-rate) as a short-term “fix”, but…

17 So What is All the Rest ? Some combination of: –True sub-monthly variability –Residual mean-field errors (particularly from very small but high-amplitude anomalies) –Data “glitches” Is the energy in these features reasonable? “Blob-by-Blob” investigation of the structure is next… Reminder - None of these signals survive the monthly gravity adjustment process. –EXCEPTING the data glitches that are edited in Level-2 Processing.


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