study of the lo calibration frequency impact on sss

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Study of the LO calibration frequency impact on SSS. C. Gabarró, V. González, J. Martínez, M. Portabella, J. Font and BEC team SMOS Barcelona Expert Centre Pg. Marítim de la Barceloneta 37-49, Barcelona SPAIN E-mail: jfont@icm.csic.es URL: www.smos-bec.icm.csic.es. Decimation study. - PowerPoint PPT Presentation

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SMOS QWG-4 – ESRIN 7-9 March 2011 1

Study of the LO calibration frequency impact on SSS

C. Gabarró, V. González, J. Martínez, M. Portabella, J. Font and BEC team

SMOS Barcelona Expert CentrePg. Marítim de la Barceloneta 37-49, Barcelona SPAINE-mail: jfont@icm.csic.esURL: www.smos-bec.icm.csic.es

SMOS QWG-4 – ESRIN 7-9 March 2011 2

Decimation study 57 full-pol semiorbits acquired at 2min and decimated at

4min, 6min, 10min (24-25 March 2010) Processors used (best available):

L1PP 3.5 L2PP 3.17

All the comparisons are relative to the 2 min LO calibration orbits. Results are not absolute values.

Example: descending Pacific orbit 20100325T040821 Global L1 data set L1 statistics over Pacific and North Atlantic Available SSS data after applying L2PP Statistics on SSS data Conclusions

SMOS QWG-4 – ESRIN 7-9 March 2011 3

Example: TB comparison @ 38-40º

20100325T040821 - descending

TBH_10min-TBH_2min TBV_10min-TBV_2min

SMOS QWG-4 – ESRIN 7-9 March 2011 4

TBH_6min-TBH_2min TBV_6min-TBV_2minExample: TB comparison @ 38-40º

SMOS QWG-4 – ESRIN 7-9 March 2011 5

TBH_4min-TBH_2min TBV_4min-TBH_2minExample: TB comparison @ 38-40º

SMOS QWG-4 – ESRIN 7-9 March 2011 6

TB differences for 1 orbit EAFTB10min-TB2min TB6min-TB2min

TB4min-TB2min

SMOS QWG-4 – ESRIN 7-9 March 2011 7

TB differences AF ONLYTB6min-TB2min AF

Very similar results for EAF or AF

TB10min-TB2min AF

TB4min-TB2min AF

SMOS QWG-4 – ESRIN 7-9 March 2011 8

Data set: TB H @ inc=38-40º

SMOS QWG-4 – ESRIN 7-9 March 2011 9

TB H @ inc=38-40º L1 RFI mask

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TB V @ inc=38-40º

SMOS QWG-4 – ESRIN 7-9 March 2011 11

TB V @ inc=38-40º L1 RFI mask

SMOS QWG-4 – ESRIN 7-9 March 2011 12

TB histogram PACIFIC area

PACIFIC dataLat=[-50,10] Lon=[-180,-100]

SMOS QWG-4 – ESRIN 7-9 March 2011 13

TB differences in PACIFIC

% TB_Nmin -TB_2min> 0.5K

TB_Nmin -TB_2min> 1K

TB_Nmin -TB_2min> 2K

N=10min 2.11% 0.27% 0.05%

N=6min 0.08% 0.03% 0.01%

N=4min 0.03% 0.01% 0.001%

PACIFICLat=[-50,10] Lon=[-180,-100]

SMOS QWG-4 – ESRIN 7-9 March 2011 14

TB histogram N. ATLANTIC area

N ATLANTIC dataLat=[30,90] Lon=[-70,0]

SMOS QWG-4 – ESRIN 7-9 March 2011 15

TB differences in N. ATLANTIC

% TB_Nmin -TB_2min> 0.5K

TB_Nmin -TB_2min> 1K

TB_Nmin -TB_2min> 2K

N=10min 17.54% 8.76% 3.87%

N=6min 5.93% 1.96% 0.46%

N=4min 1.42% 0.29% 0.053%

North ATLANTICLat=[30,90] Lon=[-70,0]

SMOS QWG-4 – ESRIN 7-9 March 2011 16

SSS data set 24-25/3/2010 57 orbAttention:Almost no clean datain N. Atlantic (L2PP filter)

SMOS QWG-4 – ESRIN 7-9 March 2011 17

SSS 24-25 march 2010 57 orbSSS 10min – 2min

SMOS QWG-4 – ESRIN 7-9 March 2011 18

SSS 24-25 march 2010 57 orbSSS 6min – 2min

SMOS QWG-4 – ESRIN 7-9 March 2011 19

SSS 24-25 march 2010 57 orbSSS 4min – 2min

SMOS QWG-4 – ESRIN 7-9 March 2011 20

Histogram SSS WORLD

Global L2OS output

When filtering byFg_poor_retrieval=1 STD (SSS10-SSS2)= 0.48 psu

SMOS QWG-4 – ESRIN 7-9 March 2011 21

Histograms SSS - PACIFIC

OnlyFg_poor_retrieval=0

SMOS QWG-4 – ESRIN 7-9 March 2011 22

Histograms SSS – N. ATLANTIC

OnlyFg_poor_retrieval=0

SMOS QWG-4 – ESRIN 7-9 March 2011 23

SSS differences: best & worst cases

% SSS_Nmin -SSS_2min> 0.2 psu

SSS_Nmin -SSS_2min> 0.5 psu

SSS_Nmin -SSS_2min>1 psu

N=10min 30.67%12.03%

9.59%2.87%

2.07%0.55%

N=6min 9.67%1.85%

1.42%0.05%

0.22%0.01%

N=4min 2.85%0.42%

0.38%0.03%

0.11%0.01%

Lat < -50º PACIFICLat=[-50,10]Lon=[-180,-110]

SMOS QWG-4 – ESRIN 7-9 March 2011 24

System requirements

R-4.5.1-008 The systematic radiometric error (including: bias, drift, periodic and other errors such as thermo-elastic effects) on the retrieved brightness temperature maps shall be lower than 1.5 K RMS at the antenna boresight and lower than 1.5´1.64 = 2.5 K RMS within 32° from boresight, after calibration

G-4.7.2-007 In order to support vicarious calibration, the system shall ensure a stability of the systematic component of the radiometric error (including: bias, drift, periodic and other errors such as thermo-elastic effects) better than 0.02 K/day.

SMOS QWG-4 – ESRIN 7-9 March 2011 25

Conclusions

The present LO calibration frequency has a clear impact on TB (larger in V-pol) and SSS.

TB differences between LO-10min and LO-2min have a global STD of 0.47 K (1.1K in N. Atlantic, 0.21 K in Pacific)

Differences in SSS (filtered by good retrieval flag): global STD 0.48 psu (0.94 psu in N. Atlantic, 0.20 psu in Pacific)

Accuracy requirement for L2 SSS is 1.2 psu. We don’t know yet the actual retrieval error, but the low calibration freq can represent in average 0.5 psu of additional error!!

SMOS SSS requirements will likely never be met with LO being calibrated at 10 min intervals

SMOS QWG-4 – ESRIN 7-9 March 2011 26

Remembering SSS requirements

R-4.6.2-004 The accuracy of the ocean salinity data products with a 50 km spatial resolution shall be <= 1.2 PSU.Note : This OS Level-2 accuracy requirement corresponds to :·  snapshot images (100) of one pixel taken during one single pass,·  usage of the narrow swath,·  full spatial coverage,·  ocean temperature of 277 K

G-4.7.2-005 The accuracy of the ocean salinity maps outside coastal areas, after averaging over 200 km x 200 km x 10 days space-time domain, shall be <= 0.1 PSU, after corrections by using vicarious calibration, namely by periodical imaging of one or more well-known reference sources.

SMOS QWG-4 – ESRIN 7-9 March 2011 27

On statistics During 10 minutes 500 SMOS snapshots are acquired Calibrating LO every 10 min means loosing 5 snapshots,

then the error in building an L3 map by averaging L2 products (wrt no calibration) increases by sqrt (500) /sqrt(495) = 1.005

Calibrating every 2 min, 25 snapshots are lost, the L3 error increases by sqrt(500)/sqrt(475) = 1.026

Going back to one orbit, the increase of usable snapshots @10 min compared to @2 min implies an error reduction of sqrt(495)/ sqrt(475) = 1.02

This 2% reduction on the required SSS error means 0.02 psu

We showed that calibrating @2 min instead of @10 min implies an error reduction by 0.2 psu (clean Pacific), 0.5 psu in global average

SMOS Barcelona Expert Centre (SMOS-BEC)Pg. Marítim de la Barceloneta 37-49, E-08003 Barcelona, SPAINTel. (+34) 93 230 95 00; Fax. (+34) 93 230 95 55URL: www.smos-bec.icm.csic.es

SMOS QWG-4 – ESRIN 7-9 March 2011 29

RFI PROBLEMS DETECTED ???

C. Gabarró, J. Martínez, V. Gonzalez, M. Portabella and BEC –TEAM

SMOS Barcelona Expert CentrePg. Marítim de la Barceloneta 37-49, Barcelona SPAINE-mail: jfont@icm.csic.esURL: www.smos-bec.icm.csic.es

SMOS QWG-4 – ESRIN 7-9 March 2011 30

RFI detected by LO cal study?

PLOT ONLY TB10min – TB2min >2K

SMOS QWG-4 – ESRIN 7-9 March 2011 31

RFI in the LO cal ?(TBH_10min –TBH_2min)>2K

(TBV_10min –TBV_2min)>2K

SMOS QWG-4 – ESRIN 7-9 March 2011 32

RFI in detector ?

Orbit ASC 20100324T0717Snapshot 20470787

SMOS QWG-4 – ESRIN 7-9 March 2011 33

RFI in detector ?

TBV LO 10min TBV LO 2min

Snapshot 20470787 Orbit ASC 20100324T0717

If TB>220 -> set to 0

SMOS QWG-4 – ESRIN 7-9 March 2011 34

RFI in the LO cal ?MASK (TBV_10min –TBV_2min)>2K

RFI TAILS??

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