Relatively cool (La Niña) conditions continued to prevail over the central and eastern tropical Pacific, and temperatures were below average over several other tropical and
subtropical oceanic regions.
Not exact matches
University of Rhode Island Estimates of contemporary global air - sea carbon dioxide (CO2) flux (Takahashi et al. 2009; Landschützer et al. 2014) suggest that
subtropical western boundary currents (WBCs) and their zonal extensions are key
regions of
oceanic carbon uptake (Figure 1a).
We see that most CO2 in the atmosphere is found above or downwind of sunny
oceanic regions beneath the
subtropical high pressure cells and those
regions migrate latitudinally to and fro with the seasons.