evaluation of microwave scatterometers and radiometers as satellite anemometers frank j. wentz,...

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Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA Workshop Satellite Measurements of Ocean Vector Winds Present Capabilities and Future Trends February 8-10, 2005

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Page 1: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA

Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers

Frank J. Wentz, Thomas Meissner, and Deborah Smith

Presented at: NOAA/NASA Workshop

Satellite Measurements of Ocean Vector WindsPresent Capabilities and Future Trends

February 8-10, 2005

Page 2: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA

Wind Direction EvaluationWindSat EDR Produced July 2004 using NOAA-NESDIS/NRL Algorithm (Jelenak)

Rain is Excluded from the Analysis

Wind Speed EvaluationCapability of Satellite Microwave Radiometers is Well Demonstrated

Midori-2 Flew both Scatterometer and Radiometer

Moored Buoys: TAO. PIRATA, NDBC, MEDS QuikScat: RSS Version NCEP FNL Analysis (GDAS)

Two Type of Evaluations

Page 3: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA

Active Versus Passive Wind Speed Retrievals:The Physics

Scatterometer measures backscatter from capillary waves (L = /(2sin) 1 cm)

Radiometer measures polarization mixing and sea foam emission

Page 4: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA

Active Versus Passive Wind Speed Retrievals:Regional Biases Eliminated

Old Sea-SurfaceEmissivity Model

New Sea-SurfaceEmissivity Model

Page 5: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA
Page 6: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA
Page 7: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA

SeaWinds and AMSR Comparison with Moored-Buoy Data

AMSR – Buoy Wind SpeedsSize: Standard Deviation

-1.5 +1.5

SeaWinds - Buoy: mean speed bias -0.12 m/s std deviation 1.1 m/s mean direction bias 1.23 deg std deviation 16.7 deg

AMSR – Buoy: mean speed bias -0.29 m/s std deviation 0.97 m/s

Page 8: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA

Conclusions On Wind Speed

The active and passive winds speed are in very close agreement. For individual observations at 25-km resolution rms difference between SeaWinds and AMSR is 0.78 m/s.

Passive wind speeds agree well with buoys (0.97 m/s standard deviation)

The passive winds are more sensitive to rain than active retrievals

The passive winds are more sensitive to nearby land

The passive winds are degraded when RFI is present (only 7 and 11 GHz so far)

Page 9: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA

The Active and Passive Directional Signal at Low Winds

Page 10: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA

Buoy Comparisons

Collocation Window = 30 minutes and 12.5 kmTriplets = WindSat + NCEP + Buoy Quadruplets = WindSat + QuikScat + NCEP + Buoy

NDBC

TAO/TRITON

PIRATA

MEDS

Page 11: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA

Before Removing >90 Outilers After Removing >90 Outliers

Num

Colloc Bias (deg)

StdDev (deg)

Num Colloc

Bias (deg)

StdDev (deg)

% Outliers

WindSat – Buoy 3084 0.86 52.82 2743 0.47 37.97 9.05 NCEP – Buoy 3084 3.33 28.71 2743 2.98 20.66 2.14 WindSat – NCEP 3084 -1.88 46.42 2743 -2.51 35.96 6.00 WindSat – Buoy 1924 0.94 54.73 1652 -0.79 39.13 10.19 QuikScat – Buoy 1924 4.31 41.31 1652 4.79 22.62 6.55 NCEP – Buoy 1924 2.45 30.30 1652 2.94 20.18 2.55 WindSat - QuikScat 1924 -4.12 56.16 1652 -4.97 38.23

Table 1: Wind direction statistics for wind speed range from 3 to 5 m/s for buoy comparisons.

Before Removing >90 Outilers After Removing >90 Outliers

Num

Colloc Bias (deg)

StdDev (deg)

Num Colloc

Bias (deg)

StdDev (deg)

% Outliers

WindSat - Buoy 13907 0.20 26.01 13676 0.03 20.95 1.56 NCEP - Buoy 13907 1.53 15.84 13676 1.66 12.67 0.37 WindSat - NCEP 13907 -1.57 23.23 13676 -1.55 19.14 0.99 WindSat - Buoy 8986 -0.93 25.10 8796 -0.97 20.82 1.35 QuikScat - Buoy 8986 2.96 21.61 8796 3.22 15.31 1.00 NCEP - Buoy 8986 1.42 15.29 8796 1.60 12.08 0.36 WindSat - QuikScat 8986 -4.66 27.81 8796 -3.99 21.49

Table 2: Wind direction statistics for wind speed range from 5 to 25 m/s for buoy comparisons.

WindSat Compared to Buoys: Tables

Page 12: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA

NC

EP

Dire

ctio

n

Win

dSat

Dire

ctio

n

Wind direction retrievals for WindSat (left) and NCEP (right) versus buoy wind direction. These results are for a wind speed range from 5-25 m/s and show the triplet collocations. A total of 1.56% of the WindSat observations and 0.37% of the NCEP values have wind directions that differ by more than 90 from the buoy direction

WindSat and NCEP Compared to Buoys

WindSat NCEP

Page 13: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA

Win

dSat

Dire

ctio

n

NC

EP

Dire

ctio

n

Qui

kSca

t D

irect

ion

WindSat, NCEP, and QuikScat Compared to Buoys

WindSat NCEP QuikScat

Page 14: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA

5-6 m/s, WindSat minus buoy rms = 28o

Standard deviation of the difference between the WindSat and buoy direction (black curve) and the QuikScat and buoy direction (red curve). These results show the quadruplet collocations for which both WindSat and QuikScat see the same buoy at nearly the same time. The faint dashed line shows the wind direction requirement of a 25-accuracy for wind speeds from 3-5 m/s and a 20-accuracy for wind speeds above 5 m/s. If either the WindSat direction or the QuikScat direction differed by more than 90 from the buoy direction, the collocation was excluded.

Head-to-Head Comparison

Page 15: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA

Before Removing >90 Outliers After Removing >90 Outliers

Num

Colloc Bias (deg)

StdDev (deg)

Num Colloc

Bias (deg)

StdDev (deg)

% Outliers

WindSat - QuikScat 4,540,548 1.8 56.6 4,036,043 1.0 41.5 11.1 QuikScat - NCEP 4,540,548 0.2 27.9 4,462,741 0.3 22.6 1.7 WindSat - NCEP 4,540,548 2.2 51.4 4,174,055 1.9 40.2 8.1

Before Removing >90 Outliers After Removing >90 Outliers

Num

Colloc Bias (deg)

StdDev (deg)

Num Colloc

Bias (deg)

StdDev (deg)

% Outliers

WindSat – QuikScat 18,965,714 0.4 24.8 18,719,480 0.2 20.5 1.3 QuikScat - NCEP 18,965,714 0.3 11.3 18,943,192 0.3 10.4 0.1 WindSat - NCEP 18,965,714 0.8 23.6 18,767,116 0.5 20.0 1.0

Table 1: Wind direction statistics for wind speed range from 3 to 5 m/s for global comparisons.

Table 2: Wind direction statistics for wind speed range from 5 to 25 m/s for global comparisons.

WindSat Compared to QuikScat: TablesCollocation Window = 60 minutes and 12.5 km

Page 16: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA

Bias (dashed curves) and standard deviation (solid curves) for wind direction differences between WindSat – NCEP (blue), WindSat – QuikScat (red) and QuikScat – NCEP (green). Outliers having directional differences greater than 90 are removed from these statistics.

WindSat Compared to QuikScat: Plots

Page 17: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA

IndividualBuoy

Histograms

W

ind

Sp

ee

d B

ias

(m

/s)

S

tdD

ev

of

Win

d S

pee

d D

iff

(m/s

)

Std

De

v o

f D

ire

cti

on

Dif

f (d

eg

)

TimeSeries

CrossTalk

Report Available containing Additional Details http://www.remss.com/support/publications.html

Assessment of the Initial Release of WindSat Wind Retrievals

Page 18: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA

Wind direction bias (dotted line) and standard deviation (solid line) for the WindSat first-ranked wind vector versus NCEP. The NOAA-NESDIS algorithm is shown in red, and the RSS algorithm is shown in blue.

New and Improved Algorithms RSS CMIS Algorithm Versus WindSat First Rank Ambiguity

NOAA\NESDIS

Page 19: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA

Radio Frequency InterferenceEuropean TV Satellites Broadcasting at 10.7 GHz

80 K ExcessBrightnessTemperature

Error in RetrievedWind Speed

Page 20: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA

CMIS Compared to WindSat

Channel Sets

WindSat CMIS 7 VH Yes Yes 7 PM No No 7 LR No No 11 VH Yes Yes 11 PM Yes No** 11 LR Yes Yes 19 VH Yes Yes 19 PM Yes Yes 19 LR Yes Yes 24 VH Yes Yes 24 PM No No 24 LR No No 37 VH Yes Yes 37 VH Yes Yes 37 VH Mute No

Page 21: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA

Radiometer Bandwidths

Band [GHz] WindSat BW [MHz] CMIS BW [MHz]

7 125 350

11 300 100

19 750 200

24 500 400

37 2000 1000

Swath WidthWindSat swath = 1000 kmCMIS swath = 1500 km

CMIS Compared to WindSat

Page 22: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA

Future Technology Advancements

Passive TechniqueInternal calibration/dedicated spacecraft allowing full 360o view2-look, fully polarimetricMarginal improvementStill limited by low winds, rain, RFI, spatial resolutionLittle or no signal below 5 m/s.

Active TechniqueDual frequency (Ku and C-band)Fully PolarimetricEnhanced spatial resolutionSignificant improvement particularly in storms and hurricanes

Page 23: Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA

Wind-direction retrieval accuracy strongly depends on wind speed

For winds less than 6 m/s, the WindSat directions error exceeds 20o

For winds above 8 m/s, WindSat accuracy close to QuikScat

New and improved algorithms may results in better performance

But, below 5 m/s there is little if any signal

RFI will be a problem for the passive technique in some areas

Rain and land effects need closer study

WindSat performance needs to be mapped to CMIS

Conclusions on Wind Direction from Passive Microwave Radiometry