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- W3136341453 abstract "Abstract The California Current System in the eastern North Pacific Ocean has experienced record high temperatures since the marine heatwave of 2014-2016. Here we show, through a compilation of data from shipboard hydrography, ocean gliders, and the Argo floats, that a high-salinity anomaly affected the California Current System from 2017-2019 in addition to the anomalously high temperatures. The salinity anomaly formed in 2015 in the North Pacific Subtropical Gyre and was subsequently advected into the California Current System, in a generation mechanism different from the events leading to the marine heatwaves of 2013/2014 and 2019 in the North Pacific. The salinity anomaly was unique in at least 16 years with an annual mean deviation from the long-term average greater than 0.2 and anomalies greater than 0.7 observed offshore. Our results imply that different source waters were found in the California Current from 2017-2019, with the near-surface California Current salinity rivaling that of the California Undercurrent." @default.
- W3136341453 created "2021-03-29" @default.
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- W3136341453 date "2021-03-19" @default.
- W3136341453 modified "2023-10-11" @default.
- W3136341453 title "Temperature and salinity extremes from 2014-2019 in the California Current System and its source waters" @default.
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- W3136341453 doi "https://doi.org/10.1038/s43247-021-00131-9" @default.
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