Climatology, trends, and future projections of aerosol optical depth over the Middle East and North Africa region in CMIP6 models

IF 3.3 Q2 ENVIRONMENTAL SCIENCES Frontiers in Climate Pub Date : 2024-07-22 DOI:10.3389/fclim.2024.1384202
R. Kunchala, Raju Attada, R. Karumuri, Vivek Seelanki, Bhupendra Bahadur Singh, Karumuri Ashok, Ibrahim Hoteit
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Abstract

This study assesses the aerosol optical depth (AOD) from historical simulations (2003–2014) and future climate scenarios (2015–2100) of the Coupled Model Intercomparison Project Phase 6 (CMIP6) over the Middle East and North Africa (MENA) region. Multi-model mean (MME) AOD statistics are generated as the average of those from the five best-performing CMIP6 models, which reproduce observational climate statistics. These models were selected based on the validation of various climate metrics, including strong pattern correlations with observations (>0.8). The resulting MME reproduces the observed AOD seasonal cycle well. The observed positive trends (summer and annual) over the Arabian Peninsula (AP) and negative trends (winter) over North Africa are well captured by MME, as regional meteorological drivers associated with observed AOD trends, with few discrepancies. Crucially, the MME fails to capture the AOD trends over North West Africa (NWA). For MENA and NWA regions, two high-emission scenarios, SSP370 and SSP585, project a continuous rise in the annual mean AOD until the end of the century. In contrast, the low-emission scenarios, SSP126 and SSP245, project a decreasing AOD trend. Interestingly, the projected future AOD area-averaged over the AP region varies significantly across all four scenarios in time. Notably, a substantial decrease of about 8–10% in the AOD is projected by the SSP126, SSP245, and SSP585 scenarios at the end of the century (2080–2100) relative to the current period. This projected decrease in annual-mean AOD, including the frequency of extreme AOD years under SSP585, is potentially associated with a concurrent increase in annual-mean rainfall over the AP.
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CMIP6 模型中中东和北非地区气溶胶光学深度的气候学、趋势和未来预测
本研究评估了中东和北非地区历史模拟(2003-2014 年)和耦合模式相互比较项目第六阶段(CMIP6)未来气候情景(2015-2100 年)的气溶胶光学深度(AOD)。多模式平均(MME)AOD 统计数据是由五个表现最好的 CMIP6 模式的平均值生成的,它们再现了观测到的气候统计数据。选择这些模式的依据是各种气候指标的验证,包括与观测数据的强模式相关性(>0.8)。由此产生的多模式模型很好地再现了观测到的 AOD 季节周期。阿拉伯半岛(AP)上空观测到的正趋势(夏季和全年)和北非上空观测到的负趋势(冬季)都被 MME 很好地捕捉到了,作为与观测到的 AOD 趋势相关的区域气象驱动因素,两者之间几乎没有差异。最关键的是,多模式气象模型未能捕捉到西北非(NWA)上空的 AOD 趋势。对于中东和北非地区以及西北非地区,SSP370 和 SSP585 这两种高排放情景预测年均 AOD 将持续上升,直到本世纪末。相比之下,低排放情景 SSP126 和 SSP245 预测 AOD 将呈下降趋势。有趣的是,在所有四种情景中,亚太地区未来的预测平均 AOD 面积在时间上有显著差异。值得注意的是,SSP126、SSP245 和 SSP585 预测本世纪末(2080-2100 年)的 AOD 将比目前大幅下降约 8-10%。预计的年均 AOD 值下降,包括 SSP585 条件下极端 AOD 年的频率下降,可能与该地区年均降雨量的同时增加有关。
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来源期刊
Frontiers in Climate
Frontiers in Climate Environmental Science-Environmental Science (miscellaneous)
CiteScore
4.50
自引率
0.00%
发文量
233
审稿时长
15 weeks
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