CMIP6 对欧亚冬季降温趋势和极端寒冷的近期和长期预测

IF 5.8 2区 环境科学与生态学 Q1 ENVIRONMENTAL SCIENCES Environmental Research Letters Pub Date : 2024-09-06 DOI:10.1088/1748-9326/ad7307
Xinping Xu, Shengping He, Botao Zhou, Bo Sun
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引用次数: 0

摘要

众所周知,气候变暖会增加气温,减少长期的极端寒冷天气。但是,内部变率对中高纬度地区的气温变率有很大的调节作用,例如,从 20 世纪 90 年代到 2010 年代初,欧亚大陆出现了显著的降温和严寒天气。未来,欧亚大陆降温和极端寒冷天气的出现是会被气候变暖抵消,还是会受到内部变率的刺激,目前仍不清楚。根据第六阶段耦合模式相互比较项目对2015-2100年的多模式预测,本研究表明,在长期(即2070-2099年),随着温室气体浓度的增加,欧亚大陆变冷趋势的预测概率从SSP126下的14.8%下降到SSP585下的0.9%。然而,在近期(即 2021-2050 年),欧亚大陆的降温现象受不同排放情景的影响较小。与整个对流层的北极深度变暖同时出现的欧亚大陆显著降温在不同情景下表现出相似的模式和强度。短期内,不同情景下北极上空对流层反气旋的相似趋势,通过向北极(中纬度)输送暖(冷)空气,促进了北极深度变暖-欧亚大陆变冷的趋势。此外,欧亚大陆冬季极寒异常(即-3.0--2.0 °C)和极寒日(即 4-6 d)在短期内对排放情景并不敏感。从长期来看,与低排放情景相比,高排放情景下气候加速变暖大大降低了欧亚大陆极端寒冷的频率和强度。因此,短期内欧亚大陆降温趋势和极端寒冷现象的发生将主要受内部影响(如乌拉尔阻塞),如果实现碳中和目标,本世纪中期以后将更多地依赖于内部变率。
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CMIP6 near-term and long-term projections of Eurasian winter cooling trend and cold extremes
It is well-known that climate warming increases air temperature and reduces cold extremes in the long-term. But internal variability strongly modulates the variability of temperature at mid- and- high latitudes, for example, causing the remarkable cooling and severe winter weather over Eurasia from the 1990s to the early 2010s. It remains unclear whether the occurrence of Eurasian cooling and cold extremes will be offset by climate warming or stimulated by internal variability in the future. Based on the Sixth phase of the Coupled Model Intercomparison Project multi-model projections for 2015–2100, this study shows that the projected probability of Eurasian cooling trend decreases with increasing greenhouse gas concentration in the long-term (i.e. 2070–2099) from 14.8% under SSP126 to 0.9% under SSP585. In the near-term (i.e. 2021–2050), however, Eurasian cooling occurrences are less influenced by different emission scenarios. Coinciding with deep Arctic warming throughout the troposphere, the projected significant Eurasian cooling exhibits similar pattern and intensity among different scenarios. The similar trend towards tropospheric anticyclone over the Arctic among different scenarios in the near-term promotes the deep Arctic warming-Eurasian cooling trend through transporting warm (cold) air into the Arctic (mid-latitudes). Moreover, winter extreme cold anomalies (i.e. −3.0–−2.0 °C) and extreme cold days (i.e. 4–6 d) over the Eurasian continent are not sensitive to emission scenarios in the near-term. In the long-term, the accelerating climate warming under high-emission scenarios significantly reduces the frequency and intensity of Eurasian cold extremes compared to low-emission scenarios. Therefore, the occurrence of Eurasian cooling trend and cold extremes in the near-term will be dominated by internal influences (e.g. Ural blocking) and will rely more on the internal variability after the mid-century if carbon neutrality goal is achieved.
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来源期刊
Environmental Research Letters
Environmental Research Letters 环境科学-环境科学
CiteScore
11.90
自引率
4.50%
发文量
763
审稿时长
4.3 months
期刊介绍: Environmental Research Letters (ERL) is a high-impact, open-access journal intended to be the meeting place of the research and policy communities concerned with environmental change and management. The journal''s coverage reflects the increasingly interdisciplinary nature of environmental science, recognizing the wide-ranging contributions to the development of methods, tools and evaluation strategies relevant to the field. Submissions from across all components of the Earth system, i.e. land, atmosphere, cryosphere, biosphere and hydrosphere, and exchanges between these components are welcome.
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