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Abstract This paper provides a comprehensive and comparative analysis of extreme precipitation patterns from 1971 to 2015 in Nepal, a data scarce, but “hot spot” region in global climate change. We compare in‐situ observations and gridded precipitation data from the Asian Precipitation Highly Resolved Observational Data Integration Toward Evaluation of Water Resources (APHRODITE). Using 11 precipitation indices, we show that high‐intensity (RX1day, R95pTOT, R99pTOT) and frequency‐related indices (R10 mm, R20 mm) have decreased but annual maximum consecutive dry and wet days have increased. Observations affirm these trends found by the APHRODITE, but show smaller magnitudes likely due to differences in measurements at locations made below the 3,000 m elevation line. Spatially, the relatively dry western region has become wetter, and the relatively wet eastern region has become drier post‐2003. The weakening of the South Asia Monsoon circulation, particularly assessed by the Webster and Yang Monsoon Index, correlates strongly with extreme precipitation indices. Changes in upper‐level jet and associated lower‐level monsoon trough are identified as critical factors influencing the extreme precipitation trend post‐2003. This study is the first to confirm the efficacy of APHRODITE in providing spatial and temporal precipitation patterns in a data‐limited region. We conclude that monsoon weakened circulations and changes in regional wind fields play dominant roles in the long‐term temporal and spatial trends of extreme precipitation in Nepal. The reduced precipitation extremes in the wet eastern region may somewhat lessen severe flooding and erosion, but the drier western region may face heightened risks in precipitation‐related hazards in Nepal.
Luo et al. (Sun,) studied this question.