it appears, for the entire tropics, the observed outgoing radiation fluxes increase with the increase in sea surface temperatures (ssts).
it appears, for the entire tropics, the observed outgoing radiation fluxes increase with the increase in sea surface temperatures (ssts).
eocene:53
using isotope proxies to determine ocean temperatures indicates sea surface temperatures in the tropics as high as 35 °c (95 °f) and, relative to present-day values, bottom water temperatures that are 10 °c (18 °f) higher.