Inherent optical properties of the ocean: Retrieval of the absorption coefficient of chromophoric dissolved organic matter from fluorescence measurements

The quantitative relationship between the absorption and fluorescence emission of chromophoric (colored) dissolved organic matter (CDOM) has been determined along five cruise tracks in the western North Atlantic Ocean, the Gulf of Mexico, and Monterey Bay, and includes Gulf Stream, Loop Current, slo...

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Published in:Limnology and Oceanography
Main Authors: Hoge, Frank E., Vodacek, Anthony, Blough, Neil V.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1993
Subjects:
Online Access:http://dx.doi.org/10.4319/lo.1993.38.7.1394
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.1993.38.7.1394
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spelling crwiley:10.4319/lo.1993.38.7.1394 2024-09-15T18:22:10+00:00 Inherent optical properties of the ocean: Retrieval of the absorption coefficient of chromophoric dissolved organic matter from fluorescence measurements Hoge, Frank E. Vodacek, Anthony Blough, Neil V. 1993 http://dx.doi.org/10.4319/lo.1993.38.7.1394 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.1993.38.7.1394 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.1993.38.7.1394 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Limnology and Oceanography volume 38, issue 7, page 1394-1402 ISSN 0024-3590 1939-5590 journal-article 1993 crwiley https://doi.org/10.4319/lo.1993.38.7.1394 2024-08-30T04:11:02Z The quantitative relationship between the absorption and fluorescence emission of chromophoric (colored) dissolved organic matter (CDOM) has been determined along five cruise tracks in the western North Atlantic Ocean, the Gulf of Mexico, and Monterey Bay, and includes Gulf Stream, Loop Current, slope, shelf, and coastal waters. We present a protocol for the determination of CDOM fluorescence that will allow both interlaboratory comparisons and the calibration of airborne fluorescence measurements. This protocol is based on the use of the water Raman signal as an internal radiometric standard and quinine sulfate as an external standard. This study demonstrates that when an appropriate and consistent procedure is used to standardize fluorescence measurements, the fluorescence per unit absorption exhibits surprisingly little variation for diverse waters. The maximum variability observed between all sites was 36% and within the western North Atlantic the variability was only 12%. Algorithms are presented for retrieval of the absorption coefficient of CDOM at 355 and 337 nm from shipboard or airborne measurements of the water‐Raman‐normalized fluorescence emission resulting from 355‐ and 337‐nm excitation. Article in Journal/Newspaper North Atlantic Wiley Online Library Limnology and Oceanography 38 7 1394 1402
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description The quantitative relationship between the absorption and fluorescence emission of chromophoric (colored) dissolved organic matter (CDOM) has been determined along five cruise tracks in the western North Atlantic Ocean, the Gulf of Mexico, and Monterey Bay, and includes Gulf Stream, Loop Current, slope, shelf, and coastal waters. We present a protocol for the determination of CDOM fluorescence that will allow both interlaboratory comparisons and the calibration of airborne fluorescence measurements. This protocol is based on the use of the water Raman signal as an internal radiometric standard and quinine sulfate as an external standard. This study demonstrates that when an appropriate and consistent procedure is used to standardize fluorescence measurements, the fluorescence per unit absorption exhibits surprisingly little variation for diverse waters. The maximum variability observed between all sites was 36% and within the western North Atlantic the variability was only 12%. Algorithms are presented for retrieval of the absorption coefficient of CDOM at 355 and 337 nm from shipboard or airborne measurements of the water‐Raman‐normalized fluorescence emission resulting from 355‐ and 337‐nm excitation.
format Article in Journal/Newspaper
author Hoge, Frank E.
Vodacek, Anthony
Blough, Neil V.
spellingShingle Hoge, Frank E.
Vodacek, Anthony
Blough, Neil V.
Inherent optical properties of the ocean: Retrieval of the absorption coefficient of chromophoric dissolved organic matter from fluorescence measurements
author_facet Hoge, Frank E.
Vodacek, Anthony
Blough, Neil V.
author_sort Hoge, Frank E.
title Inherent optical properties of the ocean: Retrieval of the absorption coefficient of chromophoric dissolved organic matter from fluorescence measurements
title_short Inherent optical properties of the ocean: Retrieval of the absorption coefficient of chromophoric dissolved organic matter from fluorescence measurements
title_full Inherent optical properties of the ocean: Retrieval of the absorption coefficient of chromophoric dissolved organic matter from fluorescence measurements
title_fullStr Inherent optical properties of the ocean: Retrieval of the absorption coefficient of chromophoric dissolved organic matter from fluorescence measurements
title_full_unstemmed Inherent optical properties of the ocean: Retrieval of the absorption coefficient of chromophoric dissolved organic matter from fluorescence measurements
title_sort inherent optical properties of the ocean: retrieval of the absorption coefficient of chromophoric dissolved organic matter from fluorescence measurements
publisher Wiley
publishDate 1993
url http://dx.doi.org/10.4319/lo.1993.38.7.1394
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.1993.38.7.1394
https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.1993.38.7.1394
genre North Atlantic
genre_facet North Atlantic
op_source Limnology and Oceanography
volume 38, issue 7, page 1394-1402
ISSN 0024-3590 1939-5590
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.4319/lo.1993.38.7.1394
container_title Limnology and Oceanography
container_volume 38
container_issue 7
container_start_page 1394
op_container_end_page 1402
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