Controls on the Activation and Strength of a High-Latitude Convective Cloud Feedback

Previous work has shown that a convective cloud feedback can greatly increase high-latitude surface temperature upon the removal of sea ice and can keep sea ice from forming throughout polar night. This feedback activates at increased greenhouse gas concentrations. It may help to explain the warm equable climates of the late Cretaceous and early Paleogene eras (similar to 100 to similar to 35 million years ago) and may be relevant for future climate under global warming. Here, the factors that determine the critical threshold CO(2) concentration at which this feedback is active and the magnitude of the warming caused by the feedback are analyzed using both a highly idealized model and NCAR's single-column atmospheric model ( SCAM) run under Arctic-like conditions. The critical CO(2) is particularly important because it helps to establish the relevance of the feedback for past and future climates. Both models agree that increased heat flux into the high latitudes at low altitudes generally decreases the critical CO(2). Increases in oceanic heat transport and in solar radiation absorbed during the summer should cause a sharp decrease in the critical CO(2), but the effect of increases in atmospheric heat transport depends on its vertical distribution. It is furthermore found (i) that if the onset of convection produces more clouds and moisture, the critical CO(2) should decrease, and the maximum temperature increase caused by the convective cloud feedback should increase and (ii) that reducing the depth of convection reduces the critical CO(2) but has little effect on the maximum temperature increase caused by the convective cloud feedback. These results should help with interpretation of the strength and onset of the convective cloud feedback as found, for example, in Intergovernmental Panel on Climate Change (IPCC) coupled ocean-atmosphere models with different cloud and convection schemes.