Abstract. The Southern Ocean (SO) region plays a critical role in the global climate system but remains observationally limited. Macquarie Island (MAC), situated along the SO storm track, provides a unique, high-quality surface precipitation record since 1948. Based on daily synoptic regime classifications from 1979 to 2023, we find that a significant 28 % increase in annual precipitation at MAC is primarily driven by enhanced mean daily precipitation intensity associated with warm air advection, low pressure, and cold air advection regimes, rather than shifts in regime frequency, consistent with a poleward shift in the storm track. In contrast, ECMWF reanalysis (ERA5) shows only an 8 % overall increase in annual precipitation, as it insufficiently reflects the increase in mean daily precipitation intensity under these regimes, likely due to its limited representation of atmospheric moisture transport and increasing evaporation. This precipitation discrepancy suggests that reanalysis may underestimate aspects of the moisture and energy budgets over the SO, and may also have potential implications for the estimation of SO freshwater fluxes.
Kong et al. (Wed,) studied this question.