scholarly journals Hysteresis conditions the vertical position of deep chlorophyll maximum in the temperate ocean

2013 ◽  
Vol 27 (4) ◽  
pp. 1013-1022 ◽  
Author(s):  
Gabriel Navarro ◽  
Javier Ruiz
Keyword(s):  
Vertical Position ◽  
Deep Chlorophyll Maximum ◽  
Chlorophyll Maximum ◽  
Temperate Ocean

Deep chlorophyll maximum (DCM) in the Red Sea

2021 ◽  
Vol 14 (3) ◽  
Author(s):  
Mohideen Wafar ◽  
Mohammad Ali Qurban ◽  
Zahid Nazeer ◽  
Karuppusamy Manikandan
Keyword(s):  
Red Sea ◽  
Deep Chlorophyll Maximum ◽  
Chlorophyll Maximum

The Deep Chlorophyll Maximum: Comparing Vertical Profiles of Chlorophyll a

1982 ◽  
Vol 39 (5) ◽  
pp. 791-803 ◽  
Author(s):  
John J. Cullen
Keyword(s):  
Chlorophyll A ◽  
Phytoplankton Biomass ◽  
Physiological Adaptation ◽  
Organic Carbon Content ◽  
Deep Chlorophyll Maximum ◽  
Vertical Profiles ◽  
In Vivo Fluorescence ◽  
Chlorophyll Maximum ◽  
Vertical Distributions

The relationship between chlorophyll a and phytoplankton biomass (organic carbon content) is highly variable as is the yield of in vivo fluorescence per unit chlorophyll. Thus, vertical profiles of chlorophyll or in vivo fluorescence must be interpreted with caution if their ecological significance is to be established. Although the variability of carbon-to-chlorophyll ratios and fluorescence yield is large, much of it can be anticipated, corrected for, and usefully interpreted. Vertical profiles from different regions of the sea are presented; each has a deep chlorophyll maximum, but the probable mechanisms of their formation and maintenance differ widely. Most vertical distributions of chlorophyll can be explained by the interaction between hydrography and growth, behavior, or physiological adaptation of phytoplankton with no special consideration of grazing by herbivores, even though vertical distributions of epizooplankton are not uniform. The interaction between vertical profiles of zooplankton and chlorophyll will be better understood when the relationships between chlorophyll and phytoplankton biomass in those profiles is determined.Key words: chlorophyll a, fluorescence, phytoplankton, vertical structure

The contribution of the deep chlorophyll maximum to primary production in a seasonally stratified shelf sea, the North Sea

2013 ◽  
Vol 113 (1-3) ◽  
pp. 153-166 ◽  
Author(s):  
Liam Fernand ◽  
Keith Weston ◽  
Tom Morris ◽  
Naomi Greenwood ◽  
Juan Brown ◽  
...  
Keyword(s):  
Primary Production ◽  
North Sea ◽  
Deep Chlorophyll Maximum ◽  
Chlorophyll Maximum ◽  
The North ◽  
Shelf Sea ◽  
The North Sea

Prochlorococcuscontributes to new production in the Sargasso Sea deep chlorophyll maximum

2007 ◽  
Vol 34 (10) ◽  
Author(s):  
John R. Casey ◽  
Michael W. Lomas ◽  
Joanna Mandecki ◽  
Donald E. Walker
Keyword(s):  
Sargasso Sea ◽  
Deep Chlorophyll Maximum ◽  
New Production ◽  
Chlorophyll Maximum

scholarly journals Primary production in the deep chlorophyll maximum of the central North Sea

2005 ◽  
Vol 27 (9) ◽  
pp. 909-922 ◽  
Author(s):  
K. Weston ◽  
L. Fernand ◽  
D. K. Mills ◽  
R. Delahunty ◽  
J. Brown
Keyword(s):  
Primary Production ◽  
North Sea ◽  
Deep Chlorophyll Maximum ◽  
Chlorophyll Maximum ◽  
Central North Sea

scholarly journals Spatio-temporal behaviour of the deep chlorophyll maximum in Mediterranean Sea: Development of a stochastic model for picophytoplankton dynamics

2013 ◽  
Vol 13 ◽  
pp. 21-34 ◽  
Author(s):  
G. Denaro ◽  
D. Valenti ◽  
A. La Cognata ◽  
B. Spagnolo ◽  
A. Bonanno ◽  
...  
Keyword(s):  
Stochastic Model ◽  
Mediterranean Sea ◽  
Deep Chlorophyll Maximum ◽  
Temporal Behaviour ◽  
Chlorophyll Maximum ◽  
Spatio Temporal

scholarly journals Mixing and the dynamics of the deep chlorophyll maximum in Lake Tahoe1

1984 ◽  
Vol 29 (4) ◽  
pp. 862-878 ◽  
Author(s):  
Mark R. Abbott ◽  
Kenneth L. Denman ◽  
Thomas M. Powell ◽  
Peter J. Richerson ◽  
Robert C. Richards ◽  
...  
Keyword(s):  
Deep Chlorophyll Maximum ◽  
Chlorophyll Maximum
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