Even as phytoplankton blooms sequester new carbon, the upwelling of deep,
subsurface water currents in the region bring old, once - sequestered carbon back to the surface waters, allowing for exchange with the atmosphere.
Not exact matches
These include eastern boundary
current upwelling systems such as those off the U.S. west coast along coastal California, Oregon and Washington, deep - sea and
subsurface oxygen minimum zones, and coastal
waters that are already experiencing excess nutrient levels (eutrophication) and low dissolved oxygen (hypoxia) due to human - driven nutrient pollution from land - based activities.
Let's see — a negative SAM --(http://curriculum.pmartineau.webfactional.com/monitoring-southern-hemisphere-stratospheric-vortex-fluctuations-and-tropospheric-coupling/)-- pushes cold
water along the Peruvian
Current to the Nino1 +2 zone dissipating the warm surface mixed layer and allowing cold
subsurface upwelling.
Then, as the La Nina of 1998/99/00 / 01 progressed, the trade winds, Pacific Equatorial
Currents, and a phenomenon known as a Rossby wave returned the remaining surface and
subsurface warm
water to the western Pacific.