Comparison of SeaWiFS and MODIS time series of inherent optical properties for the Adriatic Sea

Time series of inherent optical properties (IOPs) derived from SeaWiFS and MODIS are compared for the Adriatic Sea. The IOPs are outputs of the Quasi-Analytical Algorithm and include total absorption <i>a</i>, phytoplankton absorption <i>a</i>&...

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Main Author: F. Mélin
Format: Article
Language:English
Published: Copernicus Publications 2011-05-01
Series:Ocean Science
Online Access:http://www.ocean-sci.net/7/351/2011/os-7-351-2011.pdf
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spelling doaj-2ac7d7fc7c0e4319b541629008a072752020-11-25T02:02:55ZengCopernicus PublicationsOcean Science1812-07841812-07922011-05-017335136110.5194/os-7-351-2011Comparison of SeaWiFS and MODIS time series of inherent optical properties for the Adriatic SeaF. MélinTime series of inherent optical properties (IOPs) derived from SeaWiFS and MODIS are compared for the Adriatic Sea. The IOPs are outputs of the Quasi-Analytical Algorithm and include total absorption <i>a</i>, phytoplankton absorption <i>a</i><sub>ph</sub>, absorption associated with colored detrital material (CDM) <i>a</i><sub>cdm</sub>, and particle backscattering coefficient <i>b</i><sub>bp</sub>. The average root-mean square difference Δ computed for log-transformed distributions decreases for $a$ from 0.084 at 412 nm to 0.052 at 490 nm, is higher for <i>a</i><sub>ph</sub>(443) (0.149) than for <i>a</i><sub>cdm</sub>(443) (0.071), and is approximately 0.165 for <i>b</i><sub>bp</sub> at various wavelengths. The SeaWiFS <i>a</i> at 443 and 490 nm, <i>a</i><sub>ph</sub> at 443 nm and <i>b</i><sub>bp</sub> are on average higher than the MODIS counterparts. Statistics show significant variations in space and time. There is an overall increasing gradient for Δ associated with the absorption terms from the open southern and central Adriatic to the northwest part of the basin, and a reversed gradient for the particulate backscattering coefficient. For time series analysis, only <i>a</i>(412) and <i>a</i><sub>cdm</sub>(443) currently present an unbiased continuity bridging the SeaWiFS and MODIS periods for the Adriatic Sea.http://www.ocean-sci.net/7/351/2011/os-7-351-2011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author F. Mélin
spellingShingle F. Mélin
Comparison of SeaWiFS and MODIS time series of inherent optical properties for the Adriatic Sea
Ocean Science
author_facet F. Mélin
author_sort F. Mélin
title Comparison of SeaWiFS and MODIS time series of inherent optical properties for the Adriatic Sea
title_short Comparison of SeaWiFS and MODIS time series of inherent optical properties for the Adriatic Sea
title_full Comparison of SeaWiFS and MODIS time series of inherent optical properties for the Adriatic Sea
title_fullStr Comparison of SeaWiFS and MODIS time series of inherent optical properties for the Adriatic Sea
title_full_unstemmed Comparison of SeaWiFS and MODIS time series of inherent optical properties for the Adriatic Sea
title_sort comparison of seawifs and modis time series of inherent optical properties for the adriatic sea
publisher Copernicus Publications
series Ocean Science
issn 1812-0784
1812-0792
publishDate 2011-05-01
description Time series of inherent optical properties (IOPs) derived from SeaWiFS and MODIS are compared for the Adriatic Sea. The IOPs are outputs of the Quasi-Analytical Algorithm and include total absorption <i>a</i>, phytoplankton absorption <i>a</i><sub>ph</sub>, absorption associated with colored detrital material (CDM) <i>a</i><sub>cdm</sub>, and particle backscattering coefficient <i>b</i><sub>bp</sub>. The average root-mean square difference Δ computed for log-transformed distributions decreases for $a$ from 0.084 at 412 nm to 0.052 at 490 nm, is higher for <i>a</i><sub>ph</sub>(443) (0.149) than for <i>a</i><sub>cdm</sub>(443) (0.071), and is approximately 0.165 for <i>b</i><sub>bp</sub> at various wavelengths. The SeaWiFS <i>a</i> at 443 and 490 nm, <i>a</i><sub>ph</sub> at 443 nm and <i>b</i><sub>bp</sub> are on average higher than the MODIS counterparts. Statistics show significant variations in space and time. There is an overall increasing gradient for Δ associated with the absorption terms from the open southern and central Adriatic to the northwest part of the basin, and a reversed gradient for the particulate backscattering coefficient. For time series analysis, only <i>a</i>(412) and <i>a</i><sub>cdm</sub>(443) currently present an unbiased continuity bridging the SeaWiFS and MODIS periods for the Adriatic Sea.
url http://www.ocean-sci.net/7/351/2011/os-7-351-2011.pdf
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