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Analysis of 3 JASON cycles : Comparison of AGC and s0 Cycle 20 v. A and B Cycle 50 v. A Cycle 160 v. B AGC: Automatic gain control use to modulate the waveform amplitude MLE4 modification of the AGC /s0 relation. Rms of difference grows from 0.15 dB to 0.45dB for Ku band
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Modification of JASON rain flag for MLE4 processing
J.Tournadre 1IFREMER
• Since October 21, 2005, new Jason-1 operational processing chain for IGDR and GDR products.
• Change from MLE 3 to MLE4 retracking algorithm. • Based on a second-order altimeter echo model, MLE4
simultaneously retrieves epoch, SWH, and off-nadir angle (2).
• New instrumental corrections tables and rain flag has been updated using a Ku/C band relation computed from the first 30 version A GDR cycles.
• MLE4 algorithm is certainly more robust for large o-nadir angles,
• However, the simultaneous retrieval of and off-nadir angle significantly modifies the behavior of Ku and C band .
• Modification of the rain flagging process
Analysis of 3 JASON cycles : Comparison of AGC and s0
Cycle 20 v. A and B
Cycle 50 v. A
Cycle 160 v. B
AGC: Automatic gain control use to modulate the waveform amplitude
MLE4 modification of the AGC /s0 relation. Rms of difference grows from 0.15 dB to 0.45dB for Ku band
Sample to Sample noise
MLE 4 introduces noise in Ku signal 0.45 dB compared to 0.15dB for AGC and version A
Operational Rain flag
• Detection of significant attenuation of Ku band compared to C band
• Use of Ku/C band « rain free » relation• Criterion on JMR liquid water content Lz to insure the
presence of cloud. )5.0),(8.1max()( 0000 dBrmsf CCKu
mLz 200
Change of the Ku/C band relation
•For MLE3 and AGC Ku/C band relations are identical
•Rms at the same level.
•For MLE4 large difference for s0>15dB
•Rms 20 to 50% larger
Comparison of Ku/C band relations
Distribution of /rms
AGC/rms
Same Gaussian distribution
Impact of MLE4 on distribution5020
Version A : weak dependency of and agc on ²
Version B: strong dependency of on ²
MLE4 estimation of ² impact the Ku
Difference in rain flaggingRed dots samples flagged using the relation
Green dots: flagged using the AGC relation
For Version A AGC and flagged ensemble are only marginally different
For version B the two ensembles are statistically different
Latitudinal distributions of flagged samples
• Small difference of latitudinal distribution
Distribution of off-nadir angle for flagged samples
• Gaussian distribution slightly skew toward + values for V.A
• Larger rms and strong bias toward negative values for V.B
Solution : change from to AGC for rain flagging
• Compute the Ku/C band AGC for the whole Jason archive. Mean relation defined
• Program available for rain flagging
Rain products are also available on Cersat web site
Conclusion:• Any change modify more things than was
originally planed.