Hello,
I am working on a paleoclimate modeling project using iCESM 1.2. I have restart data from a fully coupled B case that I have been developing over the past few months, and in order to fully equilibrate the ocean while saving on computation time, I want to use this data to drive a G case that uses the same boundary conditions. I can't find much info in the user manual about how I can do this, could anyone please advise?
I am working on a paleoclimate modeling project using iCESM 1.2. I have restart data from a fully coupled B case that I have been developing over the past few months, and in order to fully equilibrate the ocean while saving on computation time, I want to use this data to drive a G case that uses the same boundary conditions. I can't find much info in the user manual about how I can do this, could anyone please advise?