An experimental technique is introduced for controlling atmospheric diabatic heating in a fully-coupled climate model (NCEP Climate Forecast System version 2), with the motivation of better understanding the role of tropical forcing in modulating the Indian summer monsoon and contributing to global seasonal prediction skill. The ‘added heating’ mechanistic approach has the benefit of not interfering with any internal model feedbacks. The approach is applied in an iterative fashion to correct bias in the three-dimensional tropical heating over the Indo-Pacific, defined as the difference between the model ensemble mean heating and that estimated from ERA-Interim. The June through September seasonal mean, trend and parabolic fit in diabatic heating are corrected for each year separately over a 20-year set of seasonal re-forecasts, resulting in a 60–90% reduction in the mean-squared error of Indo-Pacific heating from an initial set of control re-forecasts, two-thirds of which is associated with the climatological bias. This results in higher skill in the climatological mean and inter-annual variability of local low-level winds and the underlying sea surface temperature (SST). Improvements are most significant over the equatorial Indian Ocean with a removal of the climatological low-level westerly bias and SST gradient bias along with substantially more skill in inter-annual variability. Although there is very little improvement in the model rainfall over India, there is improvement in the low-level circulation. The lack of significant improvement in rainfall prediction may be partly related to the representation of convection and/or the coarse resolution grid of the model.
$\bullet$ An added heating technique is used to correct the ensemble mean atmospheric diabatic heating over the tropical Indo-Pacific in a set of climate re-forecasts.
$\bullet$ The approach in this study reduces the mean squared error in the heating by 60–90% without interfering with any internal model feedbacks.
$\bullet$ In response to heating corrections, there is significant bias correction in local low-level winds and sea surface temperature, particularly over the Indian Ocean.
$\bullet$ Despite no improvement in the simulation of rainfall over India, through teleconnections there is some improvement in the monsoon circulation.
Volume 131, 2022
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