Seasonal variability of the Black Sea Chlorophyll-a concentration
dc.contributor.author | Ivanov, Leonoid M. | |
dc.contributor.author | Margolina, Tatyana M. | |
dc.contributor.author | Chu, Peter C. | |
dc.date | 2005 | |
dc.date.accessioned | 2013-09-11T23:02:48Z | |
dc.date.available | 2013-09-11T23:02:48Z | |
dc.date.issued | 2005 | |
dc.identifier.citation | Chu, 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.uri | https://hdl.handle.net/10945/36094 | |
dc.description | Journal of Marine Systems, 56 | en_US |
dc.description | The article of record as published may be located at http://dx.doi.org/10.1016/j.jmarsys.2005.01.001 | en_US |
dc.description.abstract | The 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.rights | This 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.title | Seasonal variability of the Black Sea Chlorophyll-a concentration | en_US |
dc.type | Article | en_US |
dc.contributor.department | Oceanography | en_US |
dc.subject.author | Optimal spectral decomposition; Black Sea chlorophyll-a concentration; Subsurface chlorophyll-a maximum; Seasonal variability; Data reconstruction; Noisy and sparse data | en_US |