Oxygen gas dissolved in seawater has been studied as a tracer of physical and biological processes in the ocean for nearly half a century. Analysis of historical oxygen data has revealed widespread changes in subsurface oxygen concentrations over the past few decades, providing important constraints on the impact of late 20th century climate change on the circulation and biological productivity of the ocean. We report results from a hind cast ocean circulation/ biogeochemical model that reproduces the spatial patterns of observed subsurface O2 variability in the North Pacific, where inferred O2 trends are strongest. We find that decadal North Pacific O2 variations in the lower ventilated thermocline primarily reflect changes in the basin's large-scale circulation. A southward expansion of the model subtropical gyre explains the observed subtropical O2 increase from the 1980s to the 1990s, while the simultaneous O2 decreases seen throughout the midlatitude Pacific are driven largely by reduced communication between the atmosphere and the ocean interior. Similar O2 decreases are pervasive among mid- and high-latitude water masses, but further research is needed to determine whether these changes reflect a global response to 20th century climate change.
|Original language||English (US)|
|Number of pages||4|
|Journal||Geophysical Research Letters|
|State||Published - Aug 28 2005|
All Science Journal Classification (ASJC) codes
- Earth and Planetary Sciences(all)