Abstract

Recent decades have witnessed accelerated climate changes across the Qinghai-Tibet Plateau (QTP) and elevated socioeconomic exposure to meteorological hazards. The QTP is called the “the third pole”, exerting remarkable impact on environmental changes in its surrounding regions. While few reports are available for addressing multi-hazard risks over the QTP, we develop an integrated indicator system involving multiple meteorological hazards, i.e., droughts, rainstorms, snowstorms and hailstorms, investigating the spatiotemporal patterns of major hazards over the QTP. The hazard zones of droughts and rainstorms are identified in the southern Gangdise Mountains, the South Tibet Valley, the eastern Nyenchen-Tanglha Mountains, the Hengduan Mountains and West Sichuan Basin. Snowstorm hazard zones distribute in the Himalayas, the Bayan Har Mountains and the central Nyenchen-Tanglha Mountains, while hailstorm hazard zones cluster in central part of the QTP. Since the 21st century, intensified rainstorms are detectable in the densely populated cities of Xining and Lhasa and their adjacent areas, while amplified droughts are observed in grain production areas of the South Tibet Valley and the Hengduan Mountains. Snowstorm hazards show large interannual variations and an increase in pastoral areas, although the overall trend is declining slightly. The frequency of hailstorms gradually decreases in human settlements due to thermal and landscape effects. Mapping meteorological hazards regionalization could help to understand climate risks in the QTP, and provide scientific reference for human adaptation to climate changes in highly sensitive areas.

Highlights

  • Due to drastic climate change and the expansion of socioeconomic exposure, the disaster-related losses due to meteorological hazards have been increasing rapidly in recent decades [1,2]

  • We attempt to address the following three scientific issues: (1) What is the spatial pattern of the major meteorological hazards across the Qinghai-Tibet Plateau (QTP)? (2) How do we evaluate the integrated intensity and socioeconomic impacts of meteorological hazards? (3) Where will be the hotspots of climate risks in the QTP?

  • Historical observations suggest that the drought hazard zones are mainly distributed in the South Tibet Valley, the Nianqing-Tanggula Mountains, the Hengduan Mountains, Western Sichuan Plateau and Songpan Plateau, among which the prefectures of Xigaze, Nyingchi, Diqing, Nujiang and Aba are expected to have drought days >60 d per year (Figure 2a)

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Summary

Introduction

Due to drastic climate change and the expansion of socioeconomic exposure, the disaster-related losses due to meteorological hazards have been increasing rapidly in recent decades [1,2]. Over the past 50 years, warming magnitude of the QTP is twice as high as the global average [3,4]. A warming climate has changed the thermodynamic and kinetic conditions of the QTP [5], triggering an increase in the intensity, frequency and duration of meteorological hazards [6,7,8]. Climate projections indicate that snowstorms will continue to intensify with uncertainties and Sustainability 2021, 13, 10402.

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