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Modeled Dynamics of Physical and Biological Processes in the Central California Current System From 1993 to 2016
Author(s) -
Guo Lin,
Xiu Peng,
Chai Fei,
Chavez Francisco P.
Publication year - 2020
Publication title -
journal of geophysical research: oceans
Language(s) - English
Resource type - Journals
eISSN - 2169-9291
pISSN - 2169-9275
DOI - 10.1029/2019jc015664
Subject(s) - upwelling , ocean gyre , submarine pipeline , oceanography , nitrate , stratification (seeds) , advection , environmental science , current (fluid) , ocean current , physical oceanography , north atlantic oscillation , new production , marine ecosystem , climatology , ecosystem , atmospheric sciences , geology , nutrient , subtropics , phytoplankton , ecology , seed dormancy , botany , germination , physics , dormancy , biology , thermodynamics
A three‐dimensional physical‐biological model was used to study the dynamics of physical and biological processes in the central California Current System (CCS) from 1993 to 2016 and investigate its response to different climate modes. The variations of new production ( NP ) and nitrate fluxes in the central CCS showed robust seasonal and interannual variability. In the coastal upwelling region (0–150 km offshore), the variability of NP was associated with both coastal upwelling and alongshore nitrate advection. In the coastal transition zone (150–300 km offshore), it was related to nitrate fluxes that were determined primarily by the physics rather than nitrate concentration, with vertical mixing and offshore transport being dominant factors. In the offshore oceanic region (California Current; 300–1,000 km offshore), nitrate concentrations played a more important role in the variations of nitrate fluxes, and the NP variability was dominated by the nutrient supplies of vertical mixing and lateral transports. Although El Niño–Southern Oscillation can affect coastal upwelling, alongshore currents, and nitrate fluxes, the coastal NP responded to El Niño–Southern Oscillation mostly in the frequencies of <1 and >6 years. Pacific Decadal Oscillation and North Pacific Gyre Oscillation may affect the CCS ecosystem through large‐scale winds and stratification, modifying the circulation in the upper layer and leading to changes in nitrate concentration and NP .