基于 NEX-GDDP-CMIP6 的 21 世纪早中期亚洲干旱地区和青藏高原极端气候变化预测

IF 2.3 4区地球科学 Q3 METEOROLOGY & ATMOSPHERIC SCIENCES

Atmospheric and Oceanic Science Letters Pub Date : 2024-06-10 DOI:10.1016/j.aosl.2024.100534

Yankun Sun , Rui Zhu , Tao Wang

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It is suggested that the growth of EHT and EHP in the early subperiod of the 21st century (2026–2045) will be relatively moderate, with small differences between different emission scenarios. However, by the middle subperiod of the 21st century (2041–2060), the differences between different emission scenarios will become larger than the 2035s and the growth will become more intense. In western central Asia, TX90p, TXx, Rx5d, and R95pTOT increase by 9.7%–14.2% (13.3%–24.7%), 1.3°C–1.7°C (1.6°C–2.7°C), 6.5%–8.9% (8.2%–8.8%), and 18.1%–27.0% (25.6%–30.0%) by the early (middle) subperiod; in eastern central Asia, TX90p, TXx, Rx5d, and R95pTOT increase 8.1%–12.0% (11.3%–21.1%), 1.4°C–1.8°C (1.9°C–2.9°C), 7.4%–9.7% (10.4%–13.8%), and 20.2%–29.3% (32.0%–40.8%) by the early (middle) subperiod; and over the Tibetan Plateau, TX90p, TXx, Rx5d, and R95pTOT increase 12.5%–17.4% (17.0%–31.0%), 1.2°C–1.5°C (1.6°C–2.5°C), 7.2%–10.0% (9.9%–15.0%), and 26.6%–33.1% (36.1%–55.3%) by the early (middle) subperiod.</div><div>摘要</div><div>近年来, 随着全球变暖, 大部分地区极端气候事件的风险都有所增加. 作为中国一带一路建设核心区域的亚洲干旱区和青藏高原区域面临着严峻的极端气候风险. 本文利用NEX-GDDP-CMIP6数据预估了未来21世纪早期 (2026–2045) 和中期 (2041–2060) 不同排放情景下亚洲干旱区和青藏高原相较气候参考期 (1995–2014) 极端高温指数和极端降水指数的变化. 预估结果显示, 在不同排放情景下极端高温指数和极端降水指数都有所上升, 且在SSP5-8.5情景下增长最多, 其中NEX-GDDP-CMIP6不同模式对极端高温指数的模拟一致性高于极端降水指数. 21世纪中期相比早期极端高温指数和极端降水指数的增长更加严重.</div></div>","PeriodicalId":47210,"journal":{"name":"Atmospheric and Oceanic Science Letters","volume":"18 3","pages":"Article 100534"},"PeriodicalIF":2.3000,"publicationDate":"2024-06-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Projection of extreme climate change in the Asian arid region and the Tibetan Plateau in the early and middle 21st century based on NEX-GDDP-CMIP6\",\"authors\":\"Yankun Sun , Rui Zhu , Tao Wang\",\"doi\":\"10.1016/j.aosl.2024.100534\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>In the context of global warming, it is anticipated that both the intensity and the frequency of future global extreme high precipitation (EHP) and extreme high temperature (EHT) events will increase. 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引用次数: 0

摘要

在全球变暖的背景下，预计未来全球极端高降水（EHP）和极端高温（EHT）事件的强度和频率都将增加。为了评估未来亚洲干旱区和青藏高原的极端气候变化，本研究利用NASA地球交换全球日缩减预估（nex - gdp - cmip6），评估了21世纪不同排放情景下EHP （Rx5d和r95pto）和EHT （TX90p和TXx）的变化。结果表明，极端指数的频率和强度都将增加，在高排放情景下，特别是在SSP5-8.5排放情景下，增长速度加快。结果表明，21世纪前期（2026-2045年）EHT和EHP的增长相对温和，不同排放情景间差异不大。然而，到21世纪中期（2041-2060年），不同排放情景之间的差异将比2035年更大，增长将更加强烈。中亚西部早（中）亚期TX90p、TXx、Rx5d和r95pto分别上升9.7% ~ 14.2%（13.3% ~ 24.7%）、1.3℃~ 1.7℃（1.6℃~ 2.7℃）、6.5% ~ 8.9%（8.2% ~ 8.8%）和18.1% ~ 27.0% (25.6% ~ 30.0%)；中亚东部早（中）亚期，TX90p、TXx、Rx5d和r95pto分别上升8.1% ~ 12.0%（11.3% ~ 21.1%）、1.4°C ~ 1.8°C（1.9°C ~ 2.9°C）、7.4% ~ 9.7%（10.4% ~ 13.8%）和20.2% ~ 29.3% (32.0% ~ 40.8%)；青藏高原前期（中期）TX90p、TXx、Rx5d和R95pTOT分别上升12.5% ~ 17.4%（17.0% ~ 31.0%）、1.2℃~ 1.5℃（1.6℃~ 2.5℃）、7.2% ~ 10.0%（9.9% ~ 15.0%）和26.6% ~ 33.1%（36.1% ~ 55.3%）。摘要近年来, 随着全球变暖, 大部分地区极端气候事件的风险都有所增加. 作为中国一带一路建设核心区域的亚洲干旱区和青藏高原区域面临着严峻的极端气候风险. 本文利用NEX-GDDP-CMIP6数据预估了未来21世纪早期(2026 - 2045)和中期(2041 - 2060)不同排放情景下亚洲干旱区和青藏高原相较气候参考期(1995 - 2014)极端高温指数和极端降水指数的变化。预估结果显示,在不同排放情景下极端高温指数和极端降水指数都有所上升,且在ssp5 - 8.5情景下增长最多,其中NEX-GDDP-CMIP6不同模式对极端高温指数的模拟一致性高于极端降水指数。21世纪中期相比早期极端高温指数和极端降水指数的增长更加严重.

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Projection of extreme climate change in the Asian arid region and the Tibetan Plateau in the early and middle 21st century based on NEX-GDDP-CMIP6

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Projection of extreme climate change in the Asian arid region and the Tibetan Plateau in the early and middle 21st century based on NEX-GDDP-CMIP6

In the context of global warming, it is anticipated that both the intensity and the frequency of future global extreme high precipitation (EHP) and extreme high temperature (EHT) events will increase. To evaluate the future extreme climate changes in the Asian arid region and Tibetan Plateau, this study applied the NASA Earth Exchange Global Daily Downscaled Projections (NEX-GDDP-CMIP6) to assess the changes in EHP (Rx5d and R95pTOT) and EHT (TX90p and TXx) under different emission scenarios in the 21st century. Findings suggest that both the frequency and the intensity of the extreme indices will increase, exhibiting accelerated growth under higher emission scenarios, particularly under the SSP5-8.5 emission scenario. It is suggested that the growth of EHT and EHP in the early subperiod of the 21st century (2026–2045) will be relatively moderate, with small differences between different emission scenarios. However, by the middle subperiod of the 21st century (2041–2060), the differences between different emission scenarios will become larger than the 2035s and the growth will become more intense. In western central Asia, TX90p, TXx, Rx5d, and R95pTOT increase by 9.7%–14.2% (13.3%–24.7%), 1.3°C–1.7°C (1.6°C–2.7°C), 6.5%–8.9% (8.2%–8.8%), and 18.1%–27.0% (25.6%–30.0%) by the early (middle) subperiod; in eastern central Asia, TX90p, TXx, Rx5d, and R95pTOT increase 8.1%–12.0% (11.3%–21.1%), 1.4°C–1.8°C (1.9°C–2.9°C), 7.4%–9.7% (10.4%–13.8%), and 20.2%–29.3% (32.0%–40.8%) by the early (middle) subperiod; and over the Tibetan Plateau, TX90p, TXx, Rx5d, and R95pTOT increase 12.5%–17.4% (17.0%–31.0%), 1.2°C–1.5°C (1.6°C–2.5°C), 7.2%–10.0% (9.9%–15.0%), and 26.6%–33.1% (36.1%–55.3%) by the early (middle) subperiod.

摘要

近年来, 随着全球变暖, 大部分地区极端气候事件的风险都有所增加. 作为中国一带一路建设核心区域的亚洲干旱区和青藏高原区域面临着严峻的极端气候风险. 本文利用NEX-GDDP-CMIP6数据预估了未来21世纪早期 (2026–2045) 和中期 (2041–2060) 不同排放情景下亚洲干旱区和青藏高原相较气候参考期 (1995–2014) 极端高温指数和极端降水指数的变化. 预估结果显示, 在不同排放情景下极端高温指数和极端降水指数都有所上升, 且在SSP5-8.5情景下增长最多, 其中NEX-GDDP-CMIP6不同模式对极端高温指数的模拟一致性高于极端降水指数. 21世纪中期相比早期极端高温指数和极端降水指数的增长更加严重.

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