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Global monsoon precipitation (GMP) brings majority of water for the local agriculture and ecosystem. The Northern Hemisphere (NH) GMP shows an upward trend over the past decades, while the trend in the Southern Hemisphere (SH) GMP is weak and insignificant. The first three Singular Value Decomposition modes between NH GMP and global SST during boreal summer respectively reflect the Atlantic Multi-decadal Oscillation (AMO), Eastern Pacific (EP) ENSO, and Central Pacific (CP) ENSO, when the AMO dominates the NH climate and contributes to the increased trend. However, the first three modes between SH GMP and global SST during boreal winter are revealed as EP ENSO, the AMO, and CP ENSO, when EP ENSO becomes the most significant driver to the SH GMP and the AMO induced rainfall anomalies may cancel out with each other within the SH GM domain and thus result in a weak trend. The intensification of NH GMP is proposed to favor the occurrences of drought and heat wave (HW) in the middle latitudes through a...

Global Monsoon Precipitation: Trends, Leading Modes, and Associated Drought and Heat Wave in the Northern Hemisphere