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SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar
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SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

Dec 28, 2015

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Page 1: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

SeaWinds Empirical Rain Correction Using AMSR

January 17, 2005

Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar

Page 2: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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Outline

• Method Overview– Data set description– Variance computation change in objective function– Rain correction methods

• Performance Summary• Metrics

– Direction and Speed Histograms of DIRTH vectors– 2-D NCEP/Retrieved Relative Direction Histograms– Cross Track Bias (by liquid and speed)– Speed Bias (by liquid and speed)– RMS Direction Difference (by liquid and speed)

• Discussion

Page 3: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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Method Overview

• The entire SeaWinds mission was processed 3 ways.– Climatological attenuation correction only (SCAT)– Physically based rain correction (PHY)– Empirically based rain correction (EMP)

• The objective function was modified for all three cases. – Log(var) term was put in.– Variance was modified so that:

• assuming the standard deviation of the backscatter correction b was 50%

• noting that measurement noise was multiplied by the attenuation correction a.

varnew = a2 varold+ 0.25b

2( )

Page 4: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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Method Overview• PHY

– Uses physical models of attenuation and backscatter to compute a and b from AMSR liquid, vapor, SST, and rain rate.

– s is the splash ratio as a function of rain rate

• EMP– Estimates a and b as function of liquid, vapor, and SST

using NCEP winds collocated with SeaWinds 0 values.

– To avoid biases due to NCEP errors• Scaled a to match physical liquid=0 values.• Scaled b so that minimum backscatter was 0.

σ 0corrected = as(σ 0measured −b)

σ 0corrected = a(σ 0measured −b)

Page 5: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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Performance summary• Rain free cases are not affected significantly by the corrections.• Both rain corrections improve speed bias and reduce cross

track direction preference.• RMS direction performance is mixed

– Nearest RMS direction difference from NCEP is increased by the correction techniques, but that may be explained by:

• The number of ambiguities decreases in the corrected cases for liquids over 1 mm.

– Selected RMS direction difference has little change• One would expect improvement due to reduced cross track preference.• Lack of improvement may indicate an additional directional noise

imparted by the corrections.

– DIRTH RMS direction difference is significantly decreased especially for the empirical correction.

• DIRTH tends to smooth out directional noise in the corrected winds.

Page 6: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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Performance summary (cont)

• RMS speed performance – RMS speed differences (not shown) decrease due

to speed bias improvement– Speed variance increases; especially for the

empirical case.

Page 7: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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1-D Direction and Speed Histograms

• Plot format– NCEP Histograms were plotted together with the DIRTH

vector histograms for each correction method.– Direction and Speed Histograms were computed for varying:

• Correction Strategy (line color)

• Geographic region (plot in slide)

• Liquid Range (slide)

– Percentage of Data in each liquid range is noted.

• Observations– Corrections tend to match model direction histograms better– Corrections tend to follow model wind speed trends by

geographic region– DIRTH creates cardinal direction spikes (investigating …)

Page 8: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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Rain Free, 86% of data

Page 9: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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0.2-0.4 mm, 8.6% of data

Page 10: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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0.4-0.8 mm, 3.3% of data

Page 11: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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0.8-1.5 mm, 1.0% of data

Page 12: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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1.5-3.0 mm, 0.4% of data

Page 13: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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3.0-15 mm, 0.03% of data

Page 14: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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2-D Direction Histograms

• Two dimensional histograms of retrieved direction and NCEP direction, relative to the s/c flight direction.

• Demonstrates the removal of rain-related artifacts [e.g. cross-track directions].

• Histograms were computed for varying– Correction method (slide)– Liquid range (plot in slide)– Choice of DIRTH, Selected, or Nearest (slide)

• SCAT-only histograms repeated as the top row of each slide for comparison.– SCAT-only histograms differ for EMP and PHY slightly due

to differences in flagging.

Page 15: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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EMP, Nearest

Page 16: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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PHY, NEAREST

Page 17: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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EMP, Selected

Page 18: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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PHY, Selected

Page 19: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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EMP, DIRTH

Page 20: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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PHY, DIRTH

Page 21: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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Plot Formats

• Metrics from here on are:– Plotted as a function of

• Liquid (x-axis) (full range or 0-3 mm)– Due to a bug liquids values on the x-axis are 4 times the

true values.

• NCEP speed (multiple plots in slide)• Correction method (line color, cyan=EMP, red=PHY,

black=SCAT, dotted black=SCAT w/o log(var))

– Computed for 200 orbits of SeaWinds data.– Plots for full liquid range and 0-3 mm (99.97% of

data) are on separate slides.

Page 22: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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Speed Biases

• Metric Definition– Selected speed - NCEP speed

• Performance Summary– Nearest and DIRTH speed biases (not shown) are

similar.– Significant improvement for all but highest wind

speeds.– Even heavy rain cases show improvement.– Correction imparts little or no change for rain free

data.– Slight change in rain free biases with addition of

log(var).

Page 23: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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Speed Bias, All Liquids (Liquid x-axis values are 4X true liquid values)

Page 24: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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Speed Bias, 1-3 mm(Liquid x-axis values are 4X true liquid values)

Page 25: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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Cross Track Direction Bias

• Metric Definition– The average amount closer to the cross swath than NCEP in

degrees.• Angle between NCEP and cross swath minus the angle

between selected and cross swath.

• A positive value indicates the cross track direction is preferentially retrieved.

• Performance Summary– Corrections reduce rain induced preference for cross swath

direction.– Nearest and DIRTH performance is similar to Selected.– Full liquid range and 0-3 mm plots are shown.

Page 26: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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Cross Track Bias, All Liquids (Liquid x-axis values are 4X true liquid values)

Page 27: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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Cross Track Bias, 1-3 mm(Liquid x-axis values are 4X true liquid values)

Page 28: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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RMS Direction Difference

• Nearest, Selected, and DIRTH stats are plotted.• Performance Summary

– Correction increases Nearest RMS direction difference in rain.

• Number of ambiguities are reduced.

• Correction noise is added.

– Selected direction difference - no change• Correction noise competes with removal of cross track

preference.

– DIRTH direction difference - improvement with rain correction

• Best case DIRTH spatially smooths correction noise.

• Worst case DIRTH smooths directional features in rain.

Page 29: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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RMS Direction Diff, Nearest (Liquid x-axis values are 4X true liquid values)

Page 30: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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Number of Ambiguities (Liquid x-axis values are 4X true liquid values)

Page 31: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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RMS, Direction Diff, Selected(Liquid x-axis values are 4X true liquid values)

Page 32: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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RMS Direction Diff, DIRTH (Liquid x-axis values are 4X true liquid values)

Page 33: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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RMS Dir. Diff, DIRTH, All Liquids (Liquid x-axis values are 4X true liquid values)

Page 34: SeaWinds Empirical Rain Correction Using AMSR January 17, 2005 Bryan Stiles, Svetla Hristova-Veleva, and Scott Dunbar.

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Discussion

• What further validation is needed?• What can change analysis tell us?• Should change analysis look at:

– DIRTH solution performance?– Cross Track Direction Bias?

• What can we compare with besides NCEP? Buoys?