Articles | Volume 12, issue 4
https://doi.org/10.5194/bg-12-905-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-12-905-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
16 Feb 2015
Research article |
| 16 Feb 2015
Steady-state solutions for subsurface chlorophyll maximum in stratified water columns with a bell-shaped vertical profile of chlorophyll
X. Gong
Key Laboratory of Marine Environment and Ecology (Ministry of Education of China), Ocean University of China, Qingdao 266100, China
J. Shi
Key Laboratory of Marine Environment and Ecology (Ministry of Education of China), Ocean University of China, Qingdao 266100, China
Key Laboratory of Marine Environment and Ecology (Ministry of Education of China), Ocean University of China, Qingdao 266100, China
X. H. Yao
Key Laboratory of Marine Environment and Ecology (Ministry of Education of China), Ocean University of China, Qingdao 266100, China
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Cited
31 citations as recorded by crossref.
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- A strong summer phytoplankton bloom southeast of Vietnam in 2007, a transitional year from El Niño to La Niña H. Zhao et al. 10.1371/journal.pone.0189926
- Seasonal dynamics of seawater CO2 system at a coastal site near the southern tip of Izu Peninsula, Japan S. Wada et al. 10.1007/s10872-020-00541-x
- Formation, maintenance and diurnal variability of subsurface chlorophyll maximum during the summer monsoon in the southern Bay of Bengal R. Prasanth et al. 10.1016/j.pocean.2023.102974
- Study of the Response of Environmental Factors of the Coastal Area in Zhoushan Fishery to Typhoon In-fa Based on Remote Sensing R. Tang et al. 10.3390/rs15133349
- Contributions of physical and biogeochemical processes to phytoplankton biomass enhancement in the surface and subsurface layers during the passage of Typhoon Damrey S. Pan et al. 10.1002/2016JG003331
- Improved Perceptron of Subsurface Chlorophyll Maxima by a Deep Neural Network: A Case Study with BGC-Argo Float Data in the Northwestern Pacific Ocean J. Chen et al. 10.3390/rs14030632
- Phytoplankton Increases Induced by Tropical Cyclones in the South China Sea During 1998–2015 H. Zhao & Y. Wang 10.1002/2017JC013549
- Relative depths of the subsurface peaks of phytoplankton abundance conserved over ocean provinces M. Sato et al. 10.1002/lno.12222
- Estimation of the vertical phytoplankton distribution in the Philippine Sea: Influence of turbulence following passage of typhoons K. Cordero-Bailey et al. 10.1016/j.rsma.2022.102659
- Response of oceanic subsurface chlorophyll maxima to environmental drivers in the Northern Indian Ocean S. Garg et al. 10.1016/j.envres.2023.117528
- When Mixed Layers Are Not Mixed. Storm‐Driven Mixing and Bio‐optical Vertical Gradients in Mixed Layers of the Southern Ocean M. Carranza et al. 10.1029/2018JC014416
- Vertical variations in the bio-optical properties of seawater in the northern South China Sea during summer 2008 G. Wang et al. 10.1007/s13131-020-1535-y
- Effect of a fast‐moving tropical storm Washi on phytoplankton in the northwestern South China Sea H. Zhao et al. 10.1002/2016JC012286
- Application of functional metagenomics in the evaluation of microbial community dynamics in the Arabian Sea: Implications of environmental settings L. Khandeparker et al. 10.1016/j.jenvman.2024.123449
- Influence of Typhoon Matsa on Phytoplankton Chlorophyll-a off East China H. Zhao et al. 10.1371/journal.pone.0137863
- Algorithmic Characterization of Lake Stratification and Deep Chlorophyll Layers From Depth Profiling Water Quality Data W. Xu et al. 10.1029/2018WR023975
- What supports the deep chlorophyll maximum in acidic lakes? The role of the bacterial CO2 production in the hypolimnion S. Soria‐Píriz et al. 10.1002/lno.11391
- A mechanistic model of an upper bound on oceanic carbon export as a function of mixed layer depth and temperature Z. Li & N. Cassar 10.5194/bg-14-5015-2017
- Remote sensing observations of phytoplankton increases triggered by successive typhoons L. Huang et al. 10.1007/s11707-016-0608-x
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- Models for estimating photosynthesis parameters from in situ production profiles Ž. Kovač et al. 10.1016/j.pocean.2017.10.013
- Biogeochemical characteristics of suspended particulate matter in deep chlorophyll maximum layers in the southern East China Sea Q. Liu et al. 10.5194/bg-15-2091-2018
- Decreasing Biological Production and Carbon Export Due to the Barrier Layer: A Case Study in the Bay of Bengal H. Zhang et al. 10.3389/fmars.2021.710051
- Deep Chlorophyll Maxima in the Global Ocean: Occurrences, Drivers and Characteristics M. Cornec et al. 10.1029/2020GB006759
- Assessment of Spatial and Vertical Variability of Water Quality: Case Study of a Polymictic Polish Lake B. Ferencz & J. Dawidek 10.3390/ijerph18168620
- Vertical Variability of Total and Size-Partitioned Phytoplankton Carbon in the South China Sea W. Zheng et al. 10.3390/rs13050993
31 citations as recorded by crossref.
- A Model for the Vertical Chlorophyll-a Distribution in the Bay of Bengal Using Remote Sensing Data S. Vadakke-Chanat & P. Shanmugam 10.1109/TGRS.2019.2939548
- Evolution of 3-D chlorophyll in the northwestern Pacific Ocean using a Gaussian-activation deep neural network model X. Zhao et al. 10.3389/fmars.2024.1378488
- A strong summer phytoplankton bloom southeast of Vietnam in 2007, a transitional year from El Niño to La Niña H. Zhao et al. 10.1371/journal.pone.0189926
- Seasonal dynamics of seawater CO2 system at a coastal site near the southern tip of Izu Peninsula, Japan S. Wada et al. 10.1007/s10872-020-00541-x
- Formation, maintenance and diurnal variability of subsurface chlorophyll maximum during the summer monsoon in the southern Bay of Bengal R. Prasanth et al. 10.1016/j.pocean.2023.102974
- Study of the Response of Environmental Factors of the Coastal Area in Zhoushan Fishery to Typhoon In-fa Based on Remote Sensing R. Tang et al. 10.3390/rs15133349
- Contributions of physical and biogeochemical processes to phytoplankton biomass enhancement in the surface and subsurface layers during the passage of Typhoon Damrey S. Pan et al. 10.1002/2016JG003331
- Improved Perceptron of Subsurface Chlorophyll Maxima by a Deep Neural Network: A Case Study with BGC-Argo Float Data in the Northwestern Pacific Ocean J. Chen et al. 10.3390/rs14030632
- Phytoplankton Increases Induced by Tropical Cyclones in the South China Sea During 1998–2015 H. Zhao & Y. Wang 10.1002/2017JC013549
- Relative depths of the subsurface peaks of phytoplankton abundance conserved over ocean provinces M. Sato et al. 10.1002/lno.12222
- Estimation of the vertical phytoplankton distribution in the Philippine Sea: Influence of turbulence following passage of typhoons K. Cordero-Bailey et al. 10.1016/j.rsma.2022.102659
- Response of oceanic subsurface chlorophyll maxima to environmental drivers in the Northern Indian Ocean S. Garg et al. 10.1016/j.envres.2023.117528
- When Mixed Layers Are Not Mixed. Storm‐Driven Mixing and Bio‐optical Vertical Gradients in Mixed Layers of the Southern Ocean M. Carranza et al. 10.1029/2018JC014416
- Vertical variations in the bio-optical properties of seawater in the northern South China Sea during summer 2008 G. Wang et al. 10.1007/s13131-020-1535-y
- Effect of a fast‐moving tropical storm Washi on phytoplankton in the northwestern South China Sea H. Zhao et al. 10.1002/2016JC012286
- Application of functional metagenomics in the evaluation of microbial community dynamics in the Arabian Sea: Implications of environmental settings L. Khandeparker et al. 10.1016/j.jenvman.2024.123449
- Influence of Typhoon Matsa on Phytoplankton Chlorophyll-a off East China H. Zhao et al. 10.1371/journal.pone.0137863
- Algorithmic Characterization of Lake Stratification and Deep Chlorophyll Layers From Depth Profiling Water Quality Data W. Xu et al. 10.1029/2018WR023975
- What supports the deep chlorophyll maximum in acidic lakes? The role of the bacterial CO2 production in the hypolimnion S. Soria‐Píriz et al. 10.1002/lno.11391
- A mechanistic model of an upper bound on oceanic carbon export as a function of mixed layer depth and temperature Z. Li & N. Cassar 10.5194/bg-14-5015-2017
- Remote sensing observations of phytoplankton increases triggered by successive typhoons L. Huang et al. 10.1007/s11707-016-0608-x
- Wind‐driven currents and water masses shape spring phytoplankton distribution and composition in hydrologically complex, productive shelf waters C. Ferronato et al. 10.1002/lno.12413
- Impacts of autochthonous dissolved organic matter on the accumulation of methylmercury by phytoplankton and zooplankton in a eutrophic coastal ecosystem B. Shao et al. 10.1016/j.envpol.2023.122457
- Analytical solution of the nitracline with the evolution of subsurface chlorophyll maximum in stratified water columns X. Gong et al. 10.5194/bg-14-2371-2017
- Depth matters for bivalve culture in integrated multitrophic aquaculture (IMTA) and other polyculture strategies under non-eutrophic conditions C. Sanz-Lazaro et al. 10.1007/s10499-018-0276-9
- Models for estimating photosynthesis parameters from in situ production profiles Ž. Kovač et al. 10.1016/j.pocean.2017.10.013
- Biogeochemical characteristics of suspended particulate matter in deep chlorophyll maximum layers in the southern East China Sea Q. Liu et al. 10.5194/bg-15-2091-2018
- Decreasing Biological Production and Carbon Export Due to the Barrier Layer: A Case Study in the Bay of Bengal H. Zhang et al. 10.3389/fmars.2021.710051
- Deep Chlorophyll Maxima in the Global Ocean: Occurrences, Drivers and Characteristics M. Cornec et al. 10.1029/2020GB006759
- Assessment of Spatial and Vertical Variability of Water Quality: Case Study of a Polymictic Polish Lake B. Ferencz & J. Dawidek 10.3390/ijerph18168620
- Vertical Variability of Total and Size-Partitioned Phytoplankton Carbon in the South China Sea W. Zheng et al. 10.3390/rs13050993
Saved (final revised paper)
Latest update: 26 Dec 2024
Short summary
Analytical solutions indicate that subsurface chlorophyll maximum (SCM) occurs at or below the depth of optimal growth of phytoplankton, and the depth of SCM layer deepens logarithmically with an increase in surface light intensity; thickness and intensity of the SCM layer are mainly affected by nutrient supply, but independent of surface light intensity; intensity of the SCM strengthens as a result of this layer being shrunk by a higher light attenuation coefficient or a large sinking velocity
Analytical solutions indicate that subsurface chlorophyll maximum (SCM) occurs at or below the...
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