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Warm Events Induce Loss of Resilience in Organic Carbon Production in the Northeast Pacific Ocean
Author(s) -
Bif Mariana B.,
Siqueira Leo,
Hansell Dennis A.
Publication year - 2019
Publication title -
global biogeochemical cycles
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.512
H-Index - 187
eISSN - 1944-9224
pISSN - 0886-6236
DOI - 10.1029/2019gb006327
Subject(s) - environmental science , oceanography , biogeochemical cycle , stratification (seeds) , primary production , carbon sequestration , effects of global warming on oceans , total organic carbon , nutrient , sea surface temperature , productivity , climatology , climate change , global warming , carbon dioxide , geology , ecosystem , chemistry , dormancy , seed dormancy , ecology , botany , germination , organic chemistry , environmental chemistry , biology , macroeconomics , economics
Between 2013 and 2016, a series of warm events induced by ocean atmosphere oscillations negatively impacted productivity in the northeast Pacific Ocean. For two consecutive winters (2013–2014 and 2014–2015), suppressed wind stress and warm near‐surface ocean temperature anomalies restricted vertical mixing between the surface and underlying nutrient‐enriched waters. Here we assess historical data of sea surface temperature and sea level pressure, along with nearly a decade of biogeochemical float data to evaluate the impact of these warm events on organic carbon production. The first stratified winter experienced little apparent impact on the magnitude of net organic carbon production in the growing season relative to prior years, suggesting an immediate resilience from reduced new nutrients, apparently depending on recycled iron. However, the subsequent winter experienced virtually zero net production; a loss of resilience, perhaps due to net iron removal with export, was evident. We find that consistently enhanced winter stratification decreased carbon production much more so than a single warm winter. This study highlights the sensitivity of marine productivity to ocean atmosphere oscillations, reducing deep ocean carbon sequestration with prolonged ocean warming and stratification.