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Table 2.

Different contributions (W m−2) to the change in atmospheric cross-equatorial heat transport, where northward is positive. In the columns for the CGCM and SOM, “AGCM + x” means the value in the AGCM plus the contribution from the response. “Abs.” is short for instantaneous absorption in the atmosphere; “Adj.atm” and “Adj.cld” represent the noncloud and cloud components of rapid adjustment diagnosed in the atmosphere, respectively.

Different contributions (W m−2) to the change in atmospheric cross-equatorial heat transport, where northward is positive. In the columns for the CGCM and SOM, “AGCM + x” means the value in the AGCM plus the contribution from the response. “Abs.” is short for instantaneous absorption in the atmosphere; “Adj.atm” and “Adj.cld” represent the noncloud and cloud components of rapid adjustment diagnosed in the atmosphere, respectively.
Different contributions (W m−2) to the change in atmospheric cross-equatorial heat transport, where northward is positive. In the columns for the CGCM and SOM, “AGCM + x” means the value in the AGCM plus the contribution from the response. “Abs.” is short for instantaneous absorption in the atmosphere; “Adj.atm” and “Adj.cld” represent the noncloud and cloud components of rapid adjustment diagnosed in the atmosphere, respectively.
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