Increase the rate at which lower layers of the ocean exchanges heat with the upper layers (and thus the atmosphere). The rate at which the earth is differentially absorbing heat due to AGW is small compared to the total heat capacity of the ocean—based on current rates, we’ll get about one degree of warming in 300 years if the full heat capacity of the ocean is brought into play.
Life in the ocean depends on maintaining heat gradients. There’s a term for when the deeper layers of the ocean start mixing with warm surface and coastal waters—“algal bloom”. Algal blooms are dangerous and usually wind up killing a large amount of marine life. Among other things, this could cause global warming to become much worse.
Increase the rate at which lower layers of the ocean exchanges heat with the upper layers (and thus the atmosphere). The rate at which the earth is differentially absorbing heat due to AGW is small compared to the total heat capacity of the ocean—based on current rates, we’ll get about one degree of warming in 300 years if the full heat capacity of the ocean is brought into play.
Life in the ocean depends on maintaining heat gradients. There’s a term for when the deeper layers of the ocean start mixing with warm surface and coastal waters—“algal bloom”. Algal blooms are dangerous and usually wind up killing a large amount of marine life. Among other things, this could cause global warming to become much worse.