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www.argans.co.uk SMOS L2 Ocean Salinity Level 2 Ocean Salinity 13-14 September 2010 ARGANS & L2OS ESL
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www.argans.co.uk SMOS L2 Ocean Salinity Wind speed retrieval in Model 1 without retrieving wind direction; Dual from Full versus Full from Full ; EAFFOV versus AFFOV versus small xi-eta; Increasing threshold for valid number of measurements; Appendix;
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www.argans.co.uk SMOS L2 Ocean Salinity Model_1 retrieving WSn instead of UN10 and VN10
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www.argans.co.uk SMOS L2 Ocean Salinity Model_1 retrieving WSn instead of UN10 and VN10 Contents
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www.argans.co.uk SMOS L2 Ocean Salinity Model_1 retrieving WSn instead of UN10 and VN10
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www.argans.co.uk SMOS L2 Ocean Salinity Model_1 retrieving WSn instead of UN10 and VN10 Contents
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www.argans.co.uk SMOS L2 Ocean Salinity Model_1 retrieving WSn instead of UN10 and VN10 Contents
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www.argans.co.uk SMOS L2 Ocean Salinity Model_1 retrieving WSn instead of UN10 and VN10 Better rate of successful retrievals for the modification of Roughness Model 1 not retrieving wind direction; Much better convergence for the model with fixed wind direction; Model 1 with fixed wind direction slightly better correlates with Model 2; Retrieved Wind Speed for Model 1 with variable wind direction closer to ECMWF initial data; Recommend using Model 1 with fixed wind direction
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www.argans.co.uk SMOS L2 Ocean Salinity Dual from Full versus Full from Full
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www.argans.co.uk SMOS L2 Ocean Salinity Dual from Full versus Full from Full
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www.argans.co.uk SMOS L2 Ocean Salinity Dual from Full versus Full from Full Contents
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www.argans.co.uk SMOS L2 Ocean Salinity Dual from Full versus Full from Full More successful retrievals for Full-from-Full (FF): 74% instead of 69 %; Better convergence for FF; there are more points failed to reach convergence for DF; Better chi2 results for FF; TEC retrieval for FF has lower cross-track bias; Recommend using Full Pol from Full Pol rather than Dual Pol from Full Pol;
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www.argans.co.uk SMOS L2 Ocean Salinity EAFFOV vs AFFOV vs small xi-eta
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www.argans.co.uk SMOS L2 Ocean Salinity EAFFOV vs AFFOV vs small xi-eta Contents
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www.argans.co.uk SMOS L2 Ocean Salinity EAFFOV vs AFFOV vs small xi-eta #GP: 64790, 40733, 34467
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www.argans.co.uk SMOS L2 Ocean Salinity EAFFOV vs AFFOV vs small xi-eta
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www.argans.co.uk SMOS L2 Ocean Salinity EAFFOV vs AFFOV vs small xi-eta Contents
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www.argans.co.uk SMOS L2 Ocean Salinity EAFFOV vs AFFOV vs small xi-eta Reducing field of view decreases edge effects but does not eliminate them completely; Changing field of view does not affect significantly grid point distribution against chi2; Reducing field of view improves chi2 values, in particularly near the edges, but the edge effect is still well seen; Recommend not using AFFOV or xieta reduced instead of EAFFOV;
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www.argans.co.uk SMOS L2 Ocean Salinity Increasing threshold for valid number of measurements Extended AFFOV Threshold: 16(“min”); 30 (“low”); 50; 75
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www.argans.co.uk SMOS L2 Ocean Salinity Increasing threshold for valid number of measurements Extended AFFOV Threshold: 16(“min”); 30 (“low”); 50; 75
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www.argans.co.uk SMOS L2 Ocean Salinity Increasing threshold for valid number of measurements AFFOV Threshold: 16(“min”); 30 (“low”); 50; 75
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www.argans.co.uk SMOS L2 Ocean Salinity Increasing threshold for valid number of measurements Increasing threshold Tg_num_meas_valid sharply improves quality of results: edge effects and East-West bias are practically eliminated with a proper threshold; Increasing Tg_num_meas_valid reduces amount of available gridpoints, especially after the threshold exceeds 80-100; compromise value of the threshold should be selected, about 50-60; Effect of increasing Tg_num_meas_valid is much stronger than redaction of the field of view, from the point of reducing biases and edge effects; if we have to use FOV reduction, it could be more efficiently used in combination with increased Tg_num_meas_valid ; Recommend increasing Tg_num_meas_valid initially to 50;
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www.argans.co.uk SMOS L2 Ocean Salinity Appendix All pictures in this presentation are apparently affected/contaminated by sun that is illustrated on this slide; some results look more affected than the others – in most cases this is defined only by the colour scale used;
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