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Time scales of pattern evolution from cross-spectrum analysis of advanced very high resolution radiometer and coastal zone color scanner imagery

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Title Time scales of pattern evolution from cross-spectrum analysis of advanced very high resolution radiometer and coastal zone color scanner imagery
Names Denman, Kenneth L. (creator)
Abbott, Mark R. (creator)
Date Issued 1994 (iso8601)
Note copyrighted by American Geophysical Union
Abstract We have selected square subareas (110 km on a side) from coastal zone
color scanner (CZCS) and advanced very high resolution radiometer (AVHRR) images
for 1981 in the California Current region off northern California for which we could
identify sequences of cloud-free data over periods of days to weeks. We applied a two-dimensional
fast Fourier transform to images after median filtering, (x, y) plane
removal, and cosine tapering. We formed autospectra and coherence spectra as
functions of a scalar wavenumber. Coherence estimates between pairs of images were
plotted against time separation between images for several wide wavenumber bands to
provide a temporal lagged coherence function. The temporal rate of loss of correlation
(decorrelation time scale) in surface patterns provides a measure of the rate of pattern
change or evolution as a function of spatial dimension. We found that patterns evolved
(or lost correlation) approximately twice as rapidly in upwelling jets as in the "quieter"
regions between jets. The rapid evolution of pigment patterns (lifetime of about 1 week
or less for scales of 50-100 km) ought to hinder biomass transfer to zooplankton
predators compared with phytoplankton patches that persist for longer times. We found
no significant differences between the statistics of CZCS and AVHRR images (spectral
shape or rate of decorrelation). In addition, in two of the three areas studied, the peak
correlation between AVHRR and CZCS images from the same area occurred at zero
lag, indicating that the patterns evolved simultaneously. In the third area, maximum
coherence between thermal and pigment patterns occurred when pigment images lagged
thermal images by 1-2 days, mirroring the expected lag of high pigment behind low
temperatures (and high nutrients) in recently upwelled water. We conclude that in
dynamic areas such as coastal upwelling systems, the phytoplankton cells (identified by
pigment color patterns) behave largely as passive scalars at the mesoscale and that
growth, death, and sinking of phytoplankton collectively play at most a marginal role in
determining the spectral statistics of the pigment patterns.
Genre Article
Identifier Denman, K. L., and Abbott, M. R. , 1994, Time scales of pattern evolution from cross - spectrum analysis of advanced very high resolution radiometer and coastal zone color scanner imagery, Jour. Geophys. Res., v. 99, p. 7433 - 7442.

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