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dc.contributor.authorIvanov, Leonoid M.
dc.contributor.authorMargolina, Tatyana M.
dc.contributor.authorChu, Peter C.
dc.date2005
dc.date.accessioned2013-09-11T23:02:48Z
dc.date.available2013-09-11T23:02:48Z
dc.date.issued2005
dc.identifier.citationChu, P.C., L.M. Ivanov, and T.M. Margolina, 2005: Seasonal variability of the Black Sea Chlorophyll-a concentration (paper download). Journal of Marine Systems, 56, 243-261.
dc.identifier.urihttps://hdl.handle.net/10945/36094
dc.descriptionJournal of Marine Systems, 56en_US
dc.descriptionThe article of record as published may be located at http://dx.doi.org/10.1016/j.jmarsys.2005.01.001en_US
dc.description.abstractThe optimal spectral decomposition (OSD) method is used to reconstruct seasonal variability of the Black Sea horizontally averaged chlorophyll-a concentration from data collected during the NATO SfP-971818 Black Sea Project in 1980–1995. During the reconstruction, quality control is conducted to reduce errors caused by measurement accuracy, sampling strategy, and irregular data distribution in space and time. A bi-modal structure with winter/spring (February–March) and fall (September–October) blooms is uniquely detected and accurately documented. The chlorophyll-a enriched zone rises to 15 m depth in winter and June, and deepens to 40 m in April and 35 m in August. The June rise of the chlorophyll-a enriched zone is accompanying by near continuous reduction of upper layer maximum chlorophyll-a concentration.en_US
dc.rightsThis publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States.en_US
dc.titleSeasonal variability of the Black Sea Chlorophyll-a concentrationen_US
dc.typeArticleen_US
dc.contributor.departmentOceanographyen_US
dc.subject.authorOptimal spectral decomposition; Black Sea chlorophyll-a concentration; Subsurface chlorophyll-a maximum; Seasonal variability; Data reconstruction; Noisy and sparse dataen_US


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