Enhanced oceanic warming along the equator is also evident in the zonal means of Figure 10.6, and can be associated with oceanic heat flux changes (Watterson, 2003) and forced by the atmosphere (Liu et al., 2005).
Not exact matches
Cumulative anthropogenic carbon release of more than 5,000 Gt likely will
enhance greenhouse
warming by several degrees and substantially lower
oceanic pH values.»
The ocean as a whole is
warming; however, coastal upwelling may ultimately be
enhanced by alongshore winds, which strengthen in proportion to the temperature contrast between the
oceanic and continental air masses [Sydeman et al., 2014].
Northward atmospheric winter fluxes are observed after the
enhanced global
warming after 1970, and, for the first time over the period considered, a positive correlation is observed between atmospheric and
oceanic reducing effects on the ice extent.