Roughness model deltas v550 OTTs made from REPR v504 L1c

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Roughness model deltas v550 OTTs made from REPR v504 L1c. 30 January 2012. ARGANS. v550 OTTs made from REPR v504 L1c. OTT1-OTT2: -0.56 KOTT1-OTT3 +0.33 K. v550 OTTs made from REPR v504 L1c. OTT1-OTT2: -0.57 KOTT1-OTT3 +0.30 K. v550 OTTs made from REPR v504 L1c. - PowerPoint PPT Presentation

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www.argans.co.uk

SMOS L2 Ocean Salinity

Roughness model deltas

v550 OTTs made fromREPR v504 L1c

30 January 2012

ARGANS

www.argans.co.uk

SMOS L2 Ocean Salinity

v550 OTTs made from REPR v504 L1c

OTT1-OTT2: -0.56 K OTT1-OTT3 +0.33 K

www.argans.co.uk

SMOS L2 Ocean Salinity

v550 OTTs made from REPR v504 L1c

OTT1-OTT2: -0.57 K OTT1-OTT3 +0.30 K

www.argans.co.uk

SMOS L2 Ocean Salinity

v550 OTTs made from REPR v504 L1c

OTT1-OTT2: -0.22 K OTT1-OTT3 +0.18 K

www.argans.co.uk

SMOS L2 Ocean Salinity

v550 OTTs made from REPR v504 L1c

OTT1-OTT2: -0.22 K OTT1-OTT3 +0.19 K

www.argans.co.uk

SMOS L2 Ocean Salinity

v550 OTTs made from REPR v504 L1c

OTT1-OTT2: -0.45 K OTT1-OTT3 +0.23 K

www.argans.co.uk

SMOS L2 Ocean Salinity

v550 OTTs made from REPR v504 L1c

OTT1-OTT2: -0.45 K OTT1-OTT3 +0.22 K

www.argans.co.uk

SMOS L2 Ocean Salinity

v550 OTTs made from REPR v504 L1c

OTT1-OTT2: -0.44 K OTT1-OTT3 +0.23 K

www.argans.co.uk

SMOS L2 Ocean Salinity

v550 OTTs made from REPR v504 L1c

OTT1-OTT2: -0.43 K OTT1-OTT3 +0.20 K

www.argans.co.uk

SMOS L2 Ocean Salinity

Conclusions:

• Very small differences between ascending & descending OTT1/2/3 deltas

• Models are biased, especially in HH & in AFFOV:

OTT1-OTT2: -0.56 K OTT1-OTT3 +0.33 K OTT2-OTT3 +0.89 K

• Maybe deltas in Stokes 3 & 4 too – not tested

• Biases are corrected by OTTs

• Which model is nearer to ‘ground-truth’?

www.argans.co.uk

SMOS L2 Ocean Salinity

delta OTT1 – OTT2, descending 20111109 (event 54)

Why strong delta at top edge of VV?

www.argans.co.uk

SMOS L2 Ocean Salinity

delta OTT1 – OTT2, ascending 20111109 (event 54)

Why strong delta at top edge of VV?

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SMOS L2 Ocean Salinity

delta OTT1 – OTT2, ascending 20100704 (event 21)

Why strong delta at top edge of VV, independent of sun, ascending/descending, year, etc?

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SMOS L2 Ocean Salinity

delta OTT3 – OTT2, ascending 20100704 (event 21)

Delta at top edge in VV seems to come from model 2?

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SMOS L2 Ocean Salinity

delta OTT1 – OTT3, ascending 20100704 (event 21)

Strong gradient in HH?

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SMOS L2 Ocean Salinity

delta OTT2 – OTT3, ascending 20100704 (event 21)

Strong gradient in HH seems to come from model 3?

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SMOS L2 Ocean Salinity

delta OTT1 – OTT2, cross-pol, ascending 20100704 (event 21)

Strange pattern in Stokes 3?

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SMOS L2 Ocean Salinity

delta OTT1 – OTT2, cross-pol, ascending 20100704 (event 21)

Strange pattern in Stokes 3, hhv & vvh?

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SMOS L2 Ocean Salinity

delta OTT3 – OTT2, cross-pol, ascending 20100704 (event 21)

Strange pattern in Stokes 3, from model 2?

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SMOS L2 Ocean Salinity

Reprocessed v550 L2OS

20110704T014904, filtered by poor(retrieval or geophysical)Problem in SSS1 at edges in EAFFOV: wind/TEC/???

www.argans.co.uk

SMOS L2 Ocean Salinity

Reprocessed v550 L2OS

20110704T141932, filtered by poor(retrieval or geophysical)Problem in SSS1 at edges in EAFFOV: wind?

www.argans.co.uk

SMOS L2 Ocean Salinity

Conclusions:

• Does delta OTT1/2/3 indicate any algorithm issues?

• Does delta SSS1/2/3 in EAFFOV indicate problem with WS in SSS1?

• Why only in EAFFOV?

• Also at leading/trailing edges of snapshot inside swath, but hidden?

• How can we work towards unification of SSS1/2/3?

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