Anthropogenic aerosols are a key driver of changes in summer monsoon precipitation in the Northern Hemisphere during the 20th century. Here we apply detection and attribution methods to investigate ca
MT: mean daily temperature (°C), MaxT: maximum daily temperature (°C), MinT: minimum daily temperature (°C), P: daily precipitation (mm), W: mean wind speed (m.s-1), GR: global radiation (J.cm-2), MH:
