Predicting phytoplankton composition from space—Using the ratio of euphotic depth to mixed-layer depth: An evaluation

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dc.contributor.authorBrown, C. W.
dc.contributor.authorEsaias, W. E.
dc.contributor.authorThompson, Anne M.
dc.date.accessioned2024-07-26T16:35:03Z
dc.date.available2024-07-26T16:35:03Z
dc.date.issued1995-09-01
dc.description.abstractA technique to remotely characterize the taxonomic composition of phytoplankton would have application in several fields of environmental study. Satellite imagery available presently and in the near future will likely not be able to accomplish this, except in unique cases, using spectral methods. As an alternative approach, we empirically evaluated a technique that uses the ratio of euphotic depth (Zₑᵤ) to mixed-layer depth (Zₘ) as a parameter to predict the relative abundance of three major algal groups—diatoms, dinoflagellates, and coccolithophores— in the surface layer of the temperate North Atlantic and North Pacific Oceans. The ratio can be ascertained without in situ measurements; Zₑᵤ can be estimated from ocean color imagery, and Zₘ can be derived from hydrographic models. Diatoms were found to dominate the phytoplankton community, in terms of cell concentration, at stations possessing significantly greater values of the ration Zₑᵤ:Zₘ than those stations where dinoflagellates dominated. This is contrary to the generally accepted view that diatoms occupy less stratified water columns than dinoflagellates. The result, which may merely reflect the data set employed and as such requires further testing, could aid in classifying the phytoplankton on a regional basis. However, we conclude that the use of the ratio Zₑᵤ : Zₘ is not likely to provide a general, nonspectral technique to characterize the taxonomic composition of phytoplankton.
dc.description.sponsorshipThis work is funded through a National Research Council Postdoctoral Fellowship and an EOS Interdisciplinary Science Investigation (WHOI / MBARI / GSFC). We thank Drs. K. Baker (under Grants NASA-NAG6-14 and ONR NOOO14-81-K-0388 to R. Smith), P. Blackwelder, T. Joyce, and B. G. Mitchell, who kindly supplied the necessary components of the Warm Core Rings Experiment and Optical Dynamics Experiment data sets. We also thank Drs. K. Arrigo and J. Campbell for helpful comments and discussion, and an anonymous reviewer for useful suggestions that improved an earlier version of this manuscript.
dc.description.urihttps://www.sciencedirect.com/science/article/pii/003442579500099M
dc.format.extent5 pages
dc.genrejournal articles
dc.identifierdoi:10.13016/m2axps-hwoi
dc.identifier.citationBrown, C. W., W. E. Esaias, and A. M. Thompson. “Predicting Phytoplankton Composition from Space—Using the Ratio of Euphotic Depth to Mixed-Layer Depth: An Evaluation.” Remote Sensing of Environment 53, no. 3 (September 1, 1995): 172–76. https://doi.org/10.1016/0034-4257(95)00099-M.
dc.identifier.urihttps://doi.org/10.1016/0034-4257(95)00099-M
dc.identifier.urihttp://hdl.handle.net/11603/35057
dc.language.isoen_US
dc.publisherElsevier
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC GESTAR II
dc.rightsThis work was written as part of one of the author's official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law.
dc.rightsPublic Domain
dc.rights.urihttps://creativecommons.org/publicdomain/mark/1.0/
dc.titlePredicting phytoplankton composition from space—Using the ratio of euphotic depth to mixed-layer depth: An evaluation
dc.typeText
dcterms.creatorhttps://orcid.org/0000-0002-7829-0920

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