Three improved satellite chlorophyll algorithms for the Southern Ocean

2013 ◽  
Vol 118 (7) ◽  
pp. 3694-3703 ◽  
Author(s):  
Robert Johnson ◽  
Peter G. Strutton ◽  
Simon W. Wright ◽  
Andrew McMinn ◽  
Klaus M. Meiners
Keyword(s):  
Southern Ocean ◽  
Satellite Chlorophyll

scholarly journals Inferring source regions and supply mechanisms of iron in the Southern Ocean from satellite chlorophyll data

2015 ◽  
Vol 104 ◽  
pp. 9-25 ◽  
Author(s):  
Robert M. Graham ◽  
Agatha M. De Boer ◽  
Erik van Sebille ◽  
Karen E. Kohfeld ◽  
Christian Schlosser
Keyword(s):  
Southern Ocean ◽  
Source Regions ◽  
Satellite Chlorophyll

scholarly journals Evaluating Southern Ocean biological production in two ocean biogeochemical models on daily to seasonal time-scales using satellite surface chlorophyll and O<sub>2</sub>/Ar observations

2014 ◽  
Vol 11 (6) ◽  
pp. 9629-9665
Author(s):  
B. F. Jonsson ◽  
S. Doney ◽  
J. Dunne ◽  
M. L. Bender
Keyword(s):  
New Zealand ◽  
Southern Ocean ◽  
Time Scales ◽  
Drake Passage ◽  
Ecosystem Dynamics ◽  
Model Assessment ◽  
Biological Production ◽  
Carbon Biomass ◽  
Biogeochemical Models ◽  
Satellite Chlorophyll

Abstract. We assess the ability of ocean biogeochemical models to represent seasonal structures in biomass and net community production (NCP) in the Southern Ocean. Two models are compared to observations on daily to seasonal time scales in four different sections of the region. We use daily satellite fields of Chlorophyll (Chl) as a proxy for biomass, and in-situ observations of O2 and Ar supersaturation (ΔO2Ar) to estimate NCP. ΔO2Ar is converted to the flux of biologically generated O2 from sea to air ("O2 bioflux"). All data are aggregated to a climatological year with a daily resolution. To account for potential regional differences within the Southern Ocean, we conduct separate analyses of sections south of South Africa, around the Drake Passage, south of Australia, and south of New Zealand. We find that the models simulate the upper range of Chl concentrations well, underestimate spring levels significantly, and show differences in skill between early and late parts of the growing season. While there is a great deal of scatter in the bioflux observations in general, the four sectors each have distinct patterns that the models pick up. Neither model exhibit a significant distinction between the Australian and New Zealand sectors, and between the Drake Passage and African sectors. South of 60° S, the models fail to predict the observed extent of biological O2 undersaturation. We suggest that this shortcoming may be due either to problems with the ecosystem dynamics or problems with the vertical transport of oxygen. Overall, the bioflux observations are in general agreement with the seasonal structures in satellite chlorophyll, suggesting that this seasonality represent changes in carbon biomass and not Chl : C ratios. This agreement is shared in the models and allows us to interpret the seasonal structure of satellite chlorophyll as qualitatively reflecting the integral of biological production over time for the purposes of model assessment.

scholarly journals Evaluating Southern Ocean biological production in two ocean biogeochemical models on daily to seasonal timescales using satellite chlorophyll and O<sub>2</sub> / Ar observations

2015 ◽  
Vol 12 (3) ◽  
pp. 681-695
Author(s):  
B. F. Jonsson ◽  
S. Doney ◽  
J. Dunne ◽  
M. L. Bender
Keyword(s):  
New Zealand ◽  
Southern Ocean ◽  
Drake Passage ◽  
Ecosystem Dynamics ◽  
Net Community Production ◽  
Biogeochemical Models ◽  
In Situ Observations ◽  
Satellite Chlorophyll ◽  
Community Production

Abstract. We assess the ability of ocean biogeochemical models to represent seasonal structures in biomass and net community production (NCP) in the Southern Ocean. Two models are compared to observations on daily to seasonal timescales in four different sections of the region. We use daily satellite fields of chlorophyll (Chl) as a proxy for biomass and in situ observations of O2 and Ar supersaturation (ΔO2 / Ar) to estimate NCP. ΔO2 / Ar is converted to the flux of biologically generated O2 from sea to air (O2 bioflux). All data are aggregated to a climatological year with a daily resolution. To account for potential regional differences within the Southern Ocean, we conduct separate analyses of sections south of South Africa, around the Drake Passage, south of Australia, and south of New Zealand. We find that the models simulate the upper range of Chl concentrations well, underestimate spring levels significantly, and show differences in skill between early and late parts of the growing season. While there is a great deal of scatter in the bioflux observations in general, the four sectors each have distinct patterns that the models pick up. Neither model exhibits a significant distinction between the Australian and New Zealand sectors and between the Drake Passage and African sectors. South of 60° S, the models fail to predict the observed extent of biological O2 undersaturation. We suggest that this shortcoming may be due either to problems with the ecosystem dynamics or problems with the vertical transport of oxygen.

Prey-field use by a Southern Ocean top predator: enhanced understanding using integrated datasets

2015 ◽  
Vol 526 ◽  
pp. 169-181 ◽  
Author(s):  
M Bedford ◽  
J Melbourne-Thomas ◽  
S Corney ◽  
T Jarvis ◽  
N Kelly ◽  
...  
Keyword(s):  
Southern Ocean ◽  
Top Predator

Traits structure copepod niches in the North Atlantic and Southern Ocean

2018 ◽  
Vol 601 ◽  
pp. 109-126 ◽  
Author(s):  
N McGinty ◽  
AD Barton ◽  
NR Record ◽  
ZV Finkel ◽  
AJ Irwin
Keyword(s):  
Southern Ocean ◽  
North Atlantic ◽  
The North ◽  
The North Atlantic
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