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Daily precipitation data from the European Centre for Medium-Range Weather Forecasts (ERA-Interim) from 1979 to 2016 are analyzed to determine the trends in seasonal and extreme precipitation across the pan-Arctic and estimate the contributions to the trends from the dynamic (e.g. changes in circulation patterns) and thermodynamic processes (e.g., sea ice melt – water vapor feedback) and their interactions. The trends in the seasonal total precipitation are generally consistent with the trendsdoi:10.21203/rs.3.rs-385100/v1 fatcat:45dqvlcrfzgpzcaackubjpw2cq