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ACs processing TAO-cruise August 2006. 1. Total vs 0.2  m signal total signal 0.2  m signal The 0.2  m signal is removed from the total signal using.

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Presentation on theme: "ACs processing TAO-cruise August 2006. 1. Total vs 0.2  m signal total signal 0.2  m signal The 0.2  m signal is removed from the total signal using."— Presentation transcript:

1 ACs processing TAO-cruise August 2006

2 1. Total vs 0.2  m signal total signal 0.2  m signal The 0.2  m signal is removed from the total signal using the 0.2  m interpolated values 0.2  m interpolated values

3 2. Spectral discontinuity correction Present also in 0.2  m measurements

4 2. Spectral discontinuity correction Longer Portion of the Spectrum Shorter Portion of the Spectrum Q: Which is the correct one, LPS or SPS? A: For a p we don’t care because we know that a p (NIR)≈0.

5 2. Spectral discontinuity correction Correction method a)assume that the LPS is the correct one Longer Portion of the Spectrum

6 2. Spectral discontinuity correction Correction method a)assume that the LPS is the correct one b)using the first 2 s of the LPS, predict the value of a p at the last of the SPS

7 2. Spectral discontinuity correction Correction method a)assume that the LPS is the correct one b)using the first 2 s of the LPS, predict the value of a p at the last of the SPS c)compute the difference between the predicted and observed values of a p at the last of the SPS d)subtract such difference from the SPS

8 2. Spectral discontinuity correction Case of c p a)There is no at which we a-priori know the value of c p b)Arbitrarily assume that LSP is correct c)Apply correction as for a p d)Evaluate the bias introduced by such arbitrary assumption

9 2. Spectral discontinuity correction Bias evaluation (c p ) a)NOTE: For this data set, c p (750) (minimal values) ranges from 0.02 to 0.08 m -1 b)For most of the c p data the discontinuity is not important c)When it is important, our arbitrary assumption introduces biases of the order of 0.0007/0.02=4% (conservative estimate) d)There is no preferential direction for the shift

10 2. Spectral discontinuity correction Importance of this correction for a p a)NOTE: For this data set, a p (676) ranges from 0.001 to 0.005 m -1 b)For most of the a p data the discontinuity is not important c)When it is important, the discontinuity can be of the order of 0.0003/0.005=6% to 0.0003/0.001=30% of a p (676) d)There is no preferential direction for the shift

11 3. Interpolation to common Because the ACs produces a p and c p spectra with different wavelength centers, we interpolated each spectrum to have equally spaced values every 2 nm from 400 to 750 nm

12 4. Correction for residual T- dependence In theory by subtracting the 0.2  m interpolated signal from the total signal, we should not need any TS-correction of our a p spectra However, because the a p that we are measuring have really low values in the red region (0.001-0.005 m -1 ), even small  Ts between two consecutive 0.2  m filtrations could introduce relatively large biases in a p

13 What ranges of  T and  S are we observing between 1-hr distant data points? 4. Correction for residual T- dependence from Sullivan et al. 2006

14 4. Correction for residual T- dependence What ranges of  T and  S are we observing between 1-hr distant data points? ignore  S

15 4. Correction for residual T- dependence 1. b( ) is independent of  T (and  S) scattering correction note that part of the b-corr depends on  T 2.look at Zaneveld’s scattering correction #3:

16 4. Correction for residual T- dependence How to get  T? a)Assume that there exists a spectral region ( ref ) where: b)Set ref =710:740 nm and NIR=730 nm c)For each spectrum, find  T that minimizes: where: d)Apply T-correction to a p using the derived  T

17 4. Correction for residual T- dependence

18 no correction

19 4. Correction for residual T- dependence b-correction

20 4. Correction for residual T- dependence Tb- correction

21 4. Correction for residual T- dependence

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23 5. Compute c p T The temperature-corrected c p is finally calculated as:

24 6. Biofouling

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26 7. CD content processed ACs data merged with PAR, lat, long, SST and salinity data Sullivan et al. 2006 table interpolated every 2 nm (instrument specific)

27 Some highlights

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29 -125ºW-140ºW

30 125º140º

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33 biofouling

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