For particular regional locations (maybe we want different issues to look at different regions?), is there a relationship between temporal variability in ASC strength and cross-slope heat transport? We could look at different temporal scales (interannual, seasonal, high frequency), try different measures of ASC strength (max speed, structure, position), and different vertical integrations of cross-slope heat transport (e.g. depth integrated vs integrated over lower layers only or in certain density classes).
For particular regional locations (maybe we want different issues to look at different regions?), is there a relationship between temporal variability in ASC strength and cross-slope heat transport? We could look at different temporal scales (interannual, seasonal, high frequency), try different measures of ASC strength (max speed, structure, position), and different vertical integrations of cross-slope heat transport (e.g. depth integrated vs integrated over lower layers only or in certain density classes).