Even if there is equal warming in the tropics, but the heat is not dissipated to the poles fast
enough by the ocean currents, the area of high SSTs will increase and more heat will dissipated by other means like TC's.
Not exact matches
«Normally at the
ocean floor, at 700 meters depth, what you're accumulating is very fine material» — dust or silt small
enough that it could be carried
by currents or winds far from land without settling out.
The results are presented at a resolution high
enough to enable studying
ocean eddies and other narrow
current systems, which are overlooked
by lower - resolution models.