Role of geostrophic currents in future changes of coastal upwelling in the California Current System

Author(s):  
Hui Ding ◽  
Michael A. Alexander ◽  
Michael G. Jacox
The Condor ◽  
2000 ◽  
Vol 102 (2) ◽  
pp. 423-427 ◽  
Author(s):  
Christopher J. Hoefer

AbstractI relate marine bird density to the 55 strongest thermal fronts encountered during a survey of much of the eastern portion of the California Current and the adjacent coastal upwelling region. Elevated densities were recorded for all marine bird taxa except the Leach's Storm-Petrel (Oceanodroma leucorhoa). The variance explained by the regression models ranged from 3% for the Leach's Storm-Petrel to 85% for all marine birds. The response observed is notably stronger than previous analyses with similar data.


2005 ◽  
Vol 63 (5) ◽  
pp. 901-929 ◽  
Author(s):  
Adriana Huyer ◽  
Jane H. Fleischbein ◽  
Julie Keister ◽  
P. Michael Kosro ◽  
Natalie Perlin ◽  
...  

Ocean Science ◽  
2018 ◽  
Vol 14 (1) ◽  
pp. 69-86 ◽  
Author(s):  
Giuliana Turi ◽  
Michael Alexander ◽  
Nicole S. Lovenduski ◽  
Antonietta Capotondi ◽  
James Scott ◽  
...  

Abstract. Coastal upwelling systems, such as the California Current System (CalCS), naturally experience a wide range of O2 concentrations and pH values due to the seasonality of upwelling. Nonetheless, changes in the El Niño–Southern Oscillation (ENSO) have been shown to measurably affect the biogeochemical and physical properties of coastal upwelling regions. In this study, we use a novel, high-resolution global climate model (GFDL-ESM2.6) to investigate the influence of warm and cold ENSO events on variations in the O2 concentration and the pH of the CalCS coastal waters. An assessment of the CalCS response to six El Niño and seven La Niña events in ESM2.6 reveals significant variations in the response between events. However, these variations overlay a consistent physical and biogeochemical (O2 and pH) response in the composite mean. Focusing on the mean response, our results demonstrate that O2 and pH are affected rather differently in the euphotic zone above ∼ 100 m. The strongest O2 response reaches up to several hundreds of kilometers offshore, whereas the pH signal occurs only within a ∼ 100 km wide band along the coast. By splitting the changes in O2 and pH into individual physical and biogeochemical components that are affected by ENSO variability, we found that O2 variability in the surface ocean is primarily driven by changes in surface temperature that affect the O2 solubility. In contrast, surface pH changes are predominantly driven by changes in dissolved inorganic carbon (DIC), which in turn is affected by upwelling, explaining the confined nature of the pH signal close to the coast. Below ∼ 100 m, we find conditions with anomalously low O2 and pH, and by extension also anomalously low aragonite saturation, during La Niña. This result is consistent with findings from previous studies and highlights the stress that the CalCS ecosystem could periodically undergo in addition to impacts due to climate change.


2015 ◽  
Vol 120 (8) ◽  
pp. 5318-5341 ◽  
Author(s):  
Takeyoshi Nagai ◽  
Nicolas Gruber ◽  
Hartmut Frenzel ◽  
Zouhair Lachkar ◽  
James C. McWilliams ◽  
...  

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