Key Laboratory of Environmental Optics and Technology, Anhui Institute of Optics and Fine Mechanics, Hefei Institutes of Physical Science, Chinese Academy of Sciences, Hefei 230031, China; University of Science and Technology of China, Hefei 230026, China.
Key Laboratory of Environmental Optics and Technology, Anhui Institute of Optics and Fine Mechanics, Hefei Institutes of Physical Science, Chinese Academy of Sciences, Hefei 230031, China.
J Environ Sci (China). 2023 Oct;132:109-121. doi: 10.1016/j.jes.2022.08.030. Epub 2022 Sep 6.
Long-term stereoscopic observations of aerosol, NO, and HCHO were carried out at the Yangmeikeng (YMK) site in Shenzhen. Aerosol optical depths and NO vertical column concentration (NO VCD) derived from MAX-DOAS were found to be consistent with other datasets. The total NO VCD values of the site remained low, varying from 2 × 10 to 8 × 10 mol/cm, while the HCHO VCD was higher than NO VCD, varying from 7 × 10 to 11 × 10 mol/cm. HCHO VCD was higher from September to early November than that was from mid-late November to December and during February 2021, in contrast, NO VCD did not change much during the same period. In January, NO VCD and HCHO VCD were both fluctuating drastically. High temperature and HCHO level in the YMK site is not only driving the ozone production up but also may be driving up the ozone concentration as well, and the O production regime in the YMK site tends to be NO-limited. At various altitudes, backward trajectory clustering analysis and Potential Source Contribution Function (PSCF) were utilized to identify possible NO and HCHO source locations. The results suggested that the Huizhou-Shanwei border and the Daya Bay Sea area were the key potential source locations in the lower (200 m) and middle (500 m) atmosphere (WPSCF > 0.6). The WPSCF value was high at the 1000 m altitude which was closer to the YMK site than the near ground, indicating that the pollution transport capability in the upper atmosphere was limited.
在深圳的杨梅坑(YMK)站点进行了气溶胶、NO 和 HCHO 的长期立体观测。从 MAX-DOAS 得出的气溶胶光学深度和 NO 垂直柱浓度(NO VCD)与其他数据集一致。该站点的总 NO VCD 值一直较低,变化范围为 2×10 至 8×10 mol/cm,而 HCHO VCD 高于 NO VCD,变化范围为 7×10 至 11×10 mol/cm。与 11 月中、下旬至 12 月相比,HCHO VCD 从 9 月到 11 月初较高,而同期 NO VCD 变化不大。1 月,NO VCD 和 HCHO VCD 均急剧波动。YMK 站点的高温和 HCHO 水平不仅推动了臭氧的产生,还可能使臭氧浓度上升,YMK 站点的臭氧生成机制趋于受 NO 限制。在不同高度上,利用后向轨迹聚类分析和潜在源贡献函数(PSCF)来识别可能的 NO 和 HCHO 源位置。结果表明,惠州-汕尾边界和大亚湾海域是低层(200 m)和中层(500 m)大气中(WPSCF>0.6)的关键潜在源区。在 1000 m 高度上的 WPSCF 值较高,比近地面更接近 YMK 站点,表明高层大气中的污染传输能力有限。