scholarly journals Phytoplankton biomass and size structure across trophic gradients in the southern California Current and adjacent ocean ecosystems

2018 ◽  
Vol 592 ◽  
pp. 1-17 ◽  
Author(s):  
AG Taylor ◽  
MR Landry
1983 ◽  
Vol 76 (2) ◽  
pp. 203-211 ◽  
Author(s):  
M. Takahashi ◽  
P. K. Bienfang

2013 ◽  
Vol 22 (3) ◽  
pp. 207-219 ◽  
Author(s):  
J. Anthony Koslow ◽  
Ralf Goericke ◽  
William Watson

2018 ◽  
Vol 68 (7) ◽  
pp. 761-777 ◽  
Author(s):  
Fanny Chenillat ◽  
Peter J. S. Franks ◽  
Xavier Capet ◽  
Pascal Rivière ◽  
Nicolas Grima ◽  
...  

2019 ◽  
Vol 124 (10) ◽  
pp. 6886-6903 ◽  
Author(s):  
Laura E. Lilly ◽  
Uwe Send ◽  
Matthias Lankhorst ◽  
Todd R. Martz ◽  
Richard A. Feely ◽  
...  

2018 ◽  
Vol 63 (3) ◽  
pp. 1298-1312 ◽  
Author(s):  
Erik Askov Mousing ◽  
Katherine Richardson ◽  
Marianne Ellegaard

2005 ◽  
Vol 35 (8) ◽  
pp. 1421-1436 ◽  
Author(s):  
Niklas Schneider ◽  
Emanuele Di Lorenzo ◽  
Pearn P. Niiler

Abstract Hydrographic observations southwestward of the Southern California Bight in the period 1937–99 show that temperature and salinity variations have very different interannual variability. Temperature varies within and above the thermocline and is correlated with climate indices of El Niño, the Pacific decadal oscillation, and local upwelling. Salinity variability is largest in the surface layers of the offshore salinity minimum and is characterized by decadal-time-scale changes. The salinity anomalies are independent of temperature, of heave of the pycnocline, and of the climate indices. Calculations demonstrate that long-shore anomalous geostrophic advection of the mean salinity gradient accumulates along the mean southward trajectory along the California Current and produces the observed salinity variations. The flow anomalies for this advective process are independent of large-scale climate indices. It is hypothesized that low-frequency variability of the California Current system results from unresolved, small-scale atmospheric forcing or from the ocean mesoscale upstream of the Southern California Bight.


2020 ◽  
Vol 77 (2) ◽  
pp. 486-499 ◽  
Author(s):  
William J Sydeman ◽  
Simon Dedman ◽  
Marisol García-Reyes ◽  
Sarah Ann Thompson ◽  
Julie A Thayer ◽  
...  

Abstract The central stock of northern anchovy (CSNA; Engraulis mordax), the most abundant small pelagic fish in the southern California Current, is key to ecosystem functions. We review drivers of its population dynamics in relation to management. Springtime upwelling intensity lagged by 2 years co-varied positively with CSNA biomass, as did the abundance of Pacific sardine (Sardinops sagax; weakly negative). CSNA population dynamics indicate the need for a multi-species stock assessment, but given serious challenges with modelling population collapse and recovery dynamics, and its moderate fisheries, we suggest that sensible management could be a simple 2-tier harvest control rule designed to emphasize the key trophic role of CSNA in the ecosystem while maintaining moderate socio-economic services. We recommend a monitoring fishery of no more than 5 KMT year−1 split between central and southern California when the stock falls below the long-term median abundance estimate of 380 KMT across the California portion of its range, and a catch limit of 25 KMT year−1 when the stock is above this reference point. This rule would be precautionary, serving to maintain the most important small pelagic forage in the ecosystem, various fisheries interests, and information streams when the population is in a collapsed state.


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