We're at the end of a natural long-term cyclic temperature increase, tending to rise fast then drift down, repeating every 125,000 years or so. If AGW is significant, we may consider it beneficial to counteract trending toward the next ice age.
We're at the end of a natural long-term cyclic temperature increase, tending to rise fast then drift down, repeating every 125,000 years or so. If AGW is significant, we may consider it beneficial to counteract trending toward the next ice age.