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Interannual variability of summertime aerosol optical depth over East Asia during 2000–2011: a potential influence from El Ni?o Southern Oscillation

机译:2000-2011年东亚夏季气溶胶光学厚度的年际变化:厄尔尼诺南方涛动的潜在影响

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Aerosols degrade air quality, perturb atmospheric radiation, and impact regional and global climate. Due to the rapid increase in anthropogenic emissions, aerosol loading over East Asia (EA) is markedly higher than other industrialized regions, which motivates a need to characterize the evolution of aerosols and understand the associated drivers. Based on the MISR satellite data during 2000–2011, a wave-like interannual variation of summertime aerosol optical depth (SAOD) is observed over the highly populated North China Plain (NCP) in East Asia. Specifically, the peak-to-trough ratio of SAOD ranges from 1.4 to 1.6, with a period of 3–4 years. This variation pattern differs apparently from what has been seen in EA emissions, indicating a periodic change in regional climate pattern during the past decade.Investigations of meteorological fields over the region reveal that the high SAOD is generally associated with the enhanced Philippine Sea Anticyclone Anomaly (PSAA) which weakens southeasterlies over northeastern EA and depresses air ventilation. Alternatively, higher temperature and lower relative humidity are found to be coincident with reduced SAOD. The behavior of PSAA has been found previously to be modulated by the El Ni?o Southern Oscillations (ENSO), therefore ENSO could disturb the EA SAOD as well. Rather than changing coherently with the ENSO activity, the SAOD peaks over NCP are found to be accompanied by the rapid transition of El Ni?o warm to cold phases developed four months ahead. An index measuring the development of ENSO during January–April is able to capture the interannual variability of SAOD over NCP during 2000–2011. This finding indicates a need to integrate the large-scale periodic climate variability in the design of regional air quality policy.
机译:气溶胶会降低空气质量,扰动大气辐射,并影响区域和全球气候。由于人为排放物的迅速增加,东亚(EA)的气溶胶装载量明显高于其他工业化地区,这激发了表征气溶胶演变特征和了解相关驱动因素的需求。根据2000-2011年的MISR卫星数据,在东亚人口稠密的华北平原(NCP)上观察到了夏季气溶胶光学深度(SAOD)的波状年际变化。具体来说,SAOD的峰谷比范围为1.4到1.6,为期3-4年。这种变化模式与EA排放中的变化明显不同,表明过去十年来区域气候模式发生了周期性变化。对该区域的气象领域进行的调查显示,高SAOD通常与菲律宾海反气旋异常增强有关( PSAA)削弱了东北EA的东南风,并降低了空气流通。可替代地,发现较高的温度和较低的相对湿度与降低的SAOD一致。以前已经发现PSAA的行为受到厄尔尼诺南方涛动(ENSO)的调节,因此ENSO也可能会扰乱EA SAOD。研究发现,NCP上的SAOD峰并没有随ENSO活性的变化而一致地变化,而是伴随着四​​个月前出现的El Ni?o暖相到冷相的快速转变。衡量一月至四月ENSO发展情况的指数能够捕获2000-2011年SACP与NCP的年际变化。这一发现表明有必要将大规模的周期性气候变化纳入区域空气质量政策的设计中。

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