In addition, the authors provide compelling evidence of both the important coupling of ocean and atmosphere processes and the strong communication, of effects of climatic change, between the waters of the Northern and Southern hemisphere
through global ocean circulation.»
Not exact matches
At a
global scale, the increased melting of the ice sheet contributes to rising sea level and may impact
global ocean circulation patterns
through the so - called «thermohaline
circulation'that sustains among others, the Gulf Stream, which keeps Europe warm.
Scientists now estimate that the
circulation of seawater
through the oceanic crust accounts for 34 % of the heat input into the
global oceans, about 25 % of the globe's total heat input.
Changes in the Arctic affect the rest of the world, not only in obvious ways (such as the Arctic's contribution to sea - level rise), but
through the Arctic's role in the
global climate system, its influence on
ocean circulation, and its impacts on mid-latitude weather.
The
oceans can impact
global mean surface temperature in several ways; directly,
through surface fluxes of heat, or indirectly, by altering the atmospheric
circulation and impacting the distribution of clouds and water vapor.