研究澳大利亚东南部火绒箱干旱和黑色夏季丛林大火期间生物物理反馈对模拟极端气温的作用

IF 6.1 1区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES
Mengyuan Mu , Manon E.B. Sabot , Anna M. Ukkola , Sami W. Rifai , Martin G. De Kauwe , Sanaa Hobeichi , Andy J. Pitman
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引用次数: 0

摘要

火药桶干旱(2017-2019 年)是澳大利亚有记录以来最严重的干旱之一。极端的夏季气温(40 °C)加上干旱,导致澳大利亚东南部在 2019-20 年发生了史无前例的黑色夏季丛林大火。虽然极端气温在很大程度上是由天气过程驱动的,但了解陆地和大气之间的相互作用在多大程度上发挥了作用也很重要。在本研究中,我们使用 WRF-LIS-CABLE 陆地-大气耦合模式,通过与气候和时变 LAI 和反照率模拟对比,研究叶面积指数(LAI)和反照率变化的影响。我们分析了这些生物物理反馈对 "火绒箱干旱 "和 "黑夏丛林大火 "期间极端温度和火灾风险的影响。遥感数据显示,在干旱的三年中,澳大利亚东南沿海的 LAI(0.1-4.0 m2 m-2)与长期气候相比有所下降,而内陆的反照率则有所上升(0.02-0.14)。在 LAI 和反照率发生变化的同时,绝大多数内陆地区的日最高气温(Tmax)总体下降(降幅在 0.5 °C~),而在 2019-20 年夏季,沿海地区的日最高气温明显上升,升幅高达 1 °C。反照率的增加解释了内陆地区气温最高值下降的大部分原因,而沿海地区气温最高值的增加主要与 LAI 的下降有关。生物物理变化对气温的影响程度表明,假定植被特性固定不变的模拟可能会忽略其潜在影响。最后,我们只发现 LAI 和反照率的变化对黑夏丛林大火前的火灾风险(以燃料湿度指数衡量)影响较小,表明这些生物物理反馈并未显著调节火灾风险。我们的研究结果对依赖于气候学 LAI 和反照率的耦合模拟,包括作业天气和季节性气候预测具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Examining the role of biophysical feedbacks on simulated temperature extremes during the Tinderbox Drought and Black Summer bushfires in southeast Australia

The Tinderbox Drought (2017–2019) was one of the most severe droughts recorded in Australia. The extreme summer air temperatures (>40 °C) combined with drought, contributed to the unprecedented Black Summer bushfires in 2019–20 over southeast Australia. Whilst the temperature extremes were largely driven by synoptic processes, it is important to understand to what extent interactions between land and atmosphere played a role. In this study, we use the WRF-LIS-CABLE land-atmosphere coupled model to examine the impacts of changes in leaf area index (LAI) and albedo by contrasting simulations with climatological and time-varying LAI and albedo. We analyse the impact of these biophysical feedbacks on temperature extremes and fire risk during the Tinderbox Drought and the Black Summer bushfires. Remote-sensing data showed a decrease in LAI (0.1–4.0 m2 m−2) over the three years of the drought along the southeast coast of Australia relative to the long-term climatology, while albedo increased inland (0.02–0.14). These changes in LAI and albedo were accompanied by an overall decrease in daily maximum temperature (Tmax) in the vast majority of interior regions (by ∼0.5 °C) and, in the 2019–20 summer, by a clear increase in Tmax in the coastal regions of up to ∼1 °C. Increased albedo explained most of the decreases in Tmax inland, whereas increases in Tmax along the coasts were mostly associated with LAI declines. The magnitude of the impact of biophysical changes on temperature demonstrates the potential impact that would be missed in simulations that assumed fixed vegetation properties. Finally, we only found a small impact from LAI and albedo changes on the fire risk (as measured by the fuel moisture index) preceding the Black Summer bushfires, suggesting these biophysical feedbacks did not significantly modulate fire risk. Our results have implications for coupled simulations relying on climatological LAI and albedo, including operation weather and seasonal climate predictions.

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来源期刊
Weather and Climate Extremes
Weather and Climate Extremes Earth and Planetary Sciences-Atmospheric Science
CiteScore
11.00
自引率
7.50%
发文量
102
审稿时长
33 weeks
期刊介绍: Weather and Climate Extremes Target Audience: Academics Decision makers International development agencies Non-governmental organizations (NGOs) Civil society Focus Areas: Research in weather and climate extremes Monitoring and early warning systems Assessment of vulnerability and impacts Developing and implementing intervention policies Effective risk management and adaptation practices Engagement of local communities in adopting coping strategies Information and communication strategies tailored to local and regional needs and circumstances
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