Abstract

Twenty-five climate indices based on daily maximum and minimum temperature and precipitation at 15 meteorological stations were examined to investigate changes in temperature and precipitation extremes over the Yarlung Tsangpo River Basin (1970–2017). The trend-free prewhitening (TFPW) Mann–Kendall test and Pettitt’s test were used to identify trends and abrupt changes in the time series, respectively. The results showed widespread significant changes in extreme temperature indices associated with warming, most of which experienced abrupt changes in the 1990s. Increases in daily minimum and maximum temperature were detected, and the magnitude of daily minimum temperature change was greater than that of the daily maximum temperature, revealing an obvious decrease in the diurnal temperature range. Warm days and nights became more frequent, whereas fewer cold days and nights occurred. The frequency of frost and icing days decreased, while summer days and growing season length increased. Moreover, cold spell length shortened, whereas warm spell length increased. Additionally, changes in the precipitation extreme indices exhibited much less spatial coherence than the temperature indices. Spatially, mixed patterns of stations with positive and negative trends were found, and few trends in the precipitation extreme indices at individual stations were statistically significant. Generally, precipitation extreme indices showed a tendency toward wetter conditions, and the contribution of extreme precipitation to total precipitation has increased. However, no significant regional trends and abrupt changes were detected in total precipitation or in the frequency and duration of precipitation extremes.

Highlights

  • Global mean surface temperature rose by approximately 0.85 ◦ C during 1880–2012, and warming is projected to continue because of the future emission of greenhouse gases [1,2]

  • Maximum and minimum temperature and precipitation data were obtained from the Daily maximum and minimum temperature and precipitation data were obtained from the National Meteorological Information Centre of China

  • The overall warming trends in the extreme indices based on nighttime temperature (TN10p, TN90p, TNn, and TNx) were found in the extreme indices based on nighttime temperature (TN10p, TN90p, TNn, and TNx) were found greater than those based on daytime temperatures (TX10p, TX90p, TXn, and TXx), indicating an greater than those based on daytime temperatures (TX10p, TX90p, TXn, and TXx), indicating an obvious decrease in Diurnal Temperature Range (DTR), consistent with other regions worldwide [3,13,54,55]

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Summary

Introduction

Global mean surface temperature rose by approximately 0.85 ◦ C during 1880–2012, and warming is projected to continue because of the future emission of greenhouse gases [1,2]. Temperature and precipitation extremes have been studied both on global [3,6,11,12] and on regional scales [13,14,15,16,17]. The Yarlung Tsangpo River Basin (YTRB), which is located in southern parts of the Tibetan Plateau (TP), is known as the highest great river in the world, with a mean elevation of >4000 m above sea level [25] It contains vulnerable ecological environments and is sensitive to climate change [26]. The findings of this study, which enhance the understanding of historical changes in temperature and precipitation extremes, represent a valuable reference regarding the formulation of policies for disaster mitigation and climate change adaptation in the YTRB

Study Area
Data Source
Extreme Climate Indices and Methodology
Precipitation
Abrupt Change Analysis
Comparison with Results of Other Studies
Relationship between Extreme Precipitation Changes and Monsoon Activities
Findings
Conclusions

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