Emergence of seasonal delay of tropical rainfall during 1979-2019

Tropical rainfall exhibits cyclic north-south migration tracking the warmer hemisphere, and climate warming will delay this seasonally over land. Climate models and gridded precipitation data suggest a delay of about 4 days since 1979 is now detectable over Northern Hemisphere land and the Sahel. Tropical rainfall exhibits a prominent annual cycle, with characteristic amplitude and phase representing the range between wet and dry seasons and their onset timing, respectively. Previous studies note enhanced amplitude over ocean and delayed phase over land in model projections of global warming, underpinned by first-order physical principles. However, it is unclear whether these changes have emerged in observations. Here we use gridded precipitation datasets to report a seasonal delay of 4.1 +/- 1.1 and 4.2 +/- 0.9 days (P < 0.05) during 1979-2019 over the northern tropical land and Sahel, respectively. Most of the delay is driven by external forcings, dominated by greenhouse gases (GHG) and anthropogenic aerosols (AER). Increasing GHG and decreasing AER in the recent decades delay rainfall by producing a moister atmosphere, thus increasing its lag in response to seasonal solar forcing. As GHG increase and AER decrease, these seasonal delays are projected to further amplify in the future.

Automated summary

Recent studies have found that climate warming is causing a delay in tropical rainfall over land due to the increasing influence of greenhouse gases and anthropogenic aerosols. This delay, primarily driven by external forcings, is expected to further amplify in the future as greenhouse gases increase and aerosols decrease.