Laser remote sensing calibration of ocean color satellite data

world ocean: in fact, those processes dramatically affect the climatic equilibrium of our planet. For this reason, many advanced active and passive remote sensors have been used to study phytoplankton dynamics, since such phenomena are thought to be responsible for the sequestration of atmospheric c...

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Main Authors: N. V. Kolodnikova, L. Fiorani, F. Colao, R. Fantoni, R. Barbini, A. Palucci
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2006-06-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/3146
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spelling doaj-b32c2890811e481e8187d3be5aa5f5352020-11-25T01:59:18ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2006-06-0149110.4401/ag-3146Laser remote sensing calibration of ocean color satellite dataN. V. KolodnikovaL. FioraniF. ColaoR. FantoniR. BarbiniA. Palucciworld ocean: in fact, those processes dramatically affect the climatic equilibrium of our planet. For this reason, many advanced active and passive remote sensors have been used to study phytoplankton dynamics, since such phenomena are thought to be responsible for the sequestration of atmospheric carbon dioxide, one of the most important greenhouse gases. In this paper, one laser system and three satellite radiometers routinely used for the study of the phytoplankton dynamics will be briefly reviewed. Satellite sensors have been preferred to airborne sensors because, to our knowledge, ocean color airborne radiometers have not been operated in Antarctica, at least not throughout the whole lapse of time examined in this study. Particular focus was on the laser system (ELF) and on a specific satellite radiometer (SeaWiFS). ELF is based on the laser-induced fluorescence of phytoplankton pigments and was conceived for the Italian expeditions to Antarctica. The goal of SeaWiFS is to provide the Earth science community with quantitative data on the global ocean bio-optical properties. Such satellite radiometer has been calibrated with in situ data mainly acquired in non polar regions. This is why a comparison between ELF and SeaWiFS measurements of chlorophyll-a surface concentrations in the Southern Ocean during the austral summer 1997-1998 was believed to be significant. Our results indicate that SeaWiFS overestimates high concentrations and underestimates low concentrations. In order to correct this behavior, the chlorophyll- a bio-optical algorithm of SeaWiFS has been recalibrated according to the measurements of ELF, thus providing a new estimation of the primary production in the Southern Ocean.http://www.annalsofgeophysics.eu/index.php/annals/article/view/3146LIDAR fluorosensorsatellite radiometerSeaWiFS calibrationchlorophyll-aprimary productionAntarctica
collection DOAJ
language English
format Article
sources DOAJ
author N. V. Kolodnikova
L. Fiorani
F. Colao
R. Fantoni
R. Barbini
A. Palucci
spellingShingle N. V. Kolodnikova
L. Fiorani
F. Colao
R. Fantoni
R. Barbini
A. Palucci
Laser remote sensing calibration of ocean color satellite data
Annals of Geophysics
LIDAR fluorosensor
satellite radiometer
SeaWiFS calibration
chlorophyll-a
primary production
Antarctica
author_facet N. V. Kolodnikova
L. Fiorani
F. Colao
R. Fantoni
R. Barbini
A. Palucci
author_sort N. V. Kolodnikova
title Laser remote sensing calibration of ocean color satellite data
title_short Laser remote sensing calibration of ocean color satellite data
title_full Laser remote sensing calibration of ocean color satellite data
title_fullStr Laser remote sensing calibration of ocean color satellite data
title_full_unstemmed Laser remote sensing calibration of ocean color satellite data
title_sort laser remote sensing calibration of ocean color satellite data
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 2006-06-01
description world ocean: in fact, those processes dramatically affect the climatic equilibrium of our planet. For this reason, many advanced active and passive remote sensors have been used to study phytoplankton dynamics, since such phenomena are thought to be responsible for the sequestration of atmospheric carbon dioxide, one of the most important greenhouse gases. In this paper, one laser system and three satellite radiometers routinely used for the study of the phytoplankton dynamics will be briefly reviewed. Satellite sensors have been preferred to airborne sensors because, to our knowledge, ocean color airborne radiometers have not been operated in Antarctica, at least not throughout the whole lapse of time examined in this study. Particular focus was on the laser system (ELF) and on a specific satellite radiometer (SeaWiFS). ELF is based on the laser-induced fluorescence of phytoplankton pigments and was conceived for the Italian expeditions to Antarctica. The goal of SeaWiFS is to provide the Earth science community with quantitative data on the global ocean bio-optical properties. Such satellite radiometer has been calibrated with in situ data mainly acquired in non polar regions. This is why a comparison between ELF and SeaWiFS measurements of chlorophyll-a surface concentrations in the Southern Ocean during the austral summer 1997-1998 was believed to be significant. Our results indicate that SeaWiFS overestimates high concentrations and underestimates low concentrations. In order to correct this behavior, the chlorophyll- a bio-optical algorithm of SeaWiFS has been recalibrated according to the measurements of ELF, thus providing a new estimation of the primary production in the Southern Ocean.
topic LIDAR fluorosensor
satellite radiometer
SeaWiFS calibration
chlorophyll-a
primary production
Antarctica
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/3146
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