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| 1 | A deep stratospheric intrusion associated with an intense cut-off low event over East Asia显示文摘European Centre for Medium-Range Weather Forecasts Re-Analysis Interim(ERA-Interim)reanalysis data and satellite data,and trajectory model were applied to analyze the dynamical,thermo-dynamical,and chemical structure in the upper troposphere and lower stratosphere(UTLS)of an intense cut-off low(COL)event occurring over East Asia during June 19-23,2010,and to characterize the process and transport pathway of deep stratospheric intrusion.The Atmospheric Infrared Sounder(AIRS)ozone data and the Global Positioning System Ozone(GPSO3)sonde data showed that the air mass originating from the polar formed a region with relatively high values of potential vorticity(PV)and ozone in the center of COL,and a secondary ozone peak appeared in the upper troposphere during mature stage of the COL.Forward trajectory simulation suggested that during the first stage of COL,deep stratospheric intrusion associated with strong northerly wind jet on the west side of the upper-level trough transported ozone-rich air from the polar lower stratosphere into the middle and lower troposphere in the mid-latitude,and increased the ozone concentration there.During the mature stage of the COL,stratospheric air was transported counterclockwise into the troposphere.Backward trajectory model was used to find the source regions of air mass within the COL during its mature stage.Model results show that air masses with high ozone concentration in the center of the COL have two source regions:one is the subpolar vortex which lies in northern part of Center Siberia,where ozone-rich air plays a major role in increasing the ozone concentrations,and the other is the strong shear region which is near by the cyclonic side of the extratropical jet axis(west of 90°E,near 50°N).The air masses with low ozone concentration around the COL also have two source regions:one is the anticyclonic side of the extratropical jet axis,where the air mass with the relatively low ozone concentration at the bottom of the COL is mainly controlled by horizontal movement,and the other is the warm area of the south side of COL,where the air mass on the east and west side of the COL is mainly dominated by upward motion. | LI Dan BIAN JianChun FAN QiuJun | 2015 | Science China Earth Sciences2015，58，1： | 10 |
| 2 | Observation of a Summer Tropopause Fold by Ozonesonde at Changchun,China:Comparison with Reanalysis and Model Simulation显示文摘Tropopause folds are one of the key mechanisms of stratosphere–troposphere exchange(STE) in extratropical regions,transporting ozone-rich stratospheric air into the middle and lower troposphere. Although there have been many studies of tropopause folds that have occurred over Europe and North America,a very limited amount of work has been carried out over northeastern Asia. Ozonesondes produced by the Institute of Atmospheric Physics were launched in Changchun(43.9?N,125.2?E),Northeast China,in June 2013,and observed an ozone-enriched layer with thickness of 3 km and an ozone peak of180 ppbv at 6 km in the troposphere. The circulation field from the European Centre for Medium-Range Weather Forecasts Interim Reanalysis(ERA-Interim) dataset shows that this ozone peak was caused by a tropopause fold associated with a jet stream at the eastern flank of the East Asian trough. By analyzing the ozone data from the ozone monitoring instrument and Weather Research and Forecasting model with Chemistry(WRF-Chem) simulations,it was found that a high ozone concentration tongue originating from the lower stratosphere at high latitude(near central Siberia) intruded into the middle troposphere over Changchun between 5 and 8 km on 12 June 2013. The high-resolution WRF-Chem simulation was capable of describing events such as the tropopause fold that occurred on the cyclonic shear side of the jet stream. In addition,the TRAJ3 D trajectory model was used to trace the origin of measured secondary ozone peaks in the middle troposphere back,for example,to stratospheric intrusion through the tropopause fold. | LI Dan BIAN Jianchun | 2015 | Advances in Atmospheric Sciences2015，32，10： | 8 |
| 3 | 东亚一次典型切断低压引起的平流层空气深入侵过程的分析显示文摘利用ERA-Interim再分析资料、卫星资料以及轨迹模式,对2010年6月19-23日东亚夏季一次典型切断低压(COL)过程中的动力、热力及化学结构进行了分析,并详细分析了平流层空气深入侵过程和路径.AIRS臭氧资料与臭氧探空资料分析表明,在COL发展成熟阶段,由极区高位势涡度、高臭氧库区脱离出来的空气在COL的中心形成一个局地高位势涡度与高臭氧浓度区域,并在对流层中上部出现臭氧次峰结构.前向轨迹模式模拟结果表明:COL形成前期,高空槽加深,槽后偏北风急流可以引起极区下平流层空气向中纬度对流层中低层侵入,从而使对流层中低层臭氧浓度升高;COL发展成熟阶段,可以引起平流层空气的"旋转式"入侵.最后,应用后向轨迹模式对成熟阶段COL内部及周围空气块源地做进一步模拟分析.结果表明:(1)COL中心高浓度臭氧空气块源地有两个,一是中西伯利亚北部上空的副极地涡旋,这部分气块对COL中心的高臭氧浓度起主要作用;二是90°E以西,50°N附近的温带急流轴左侧的气旋式风速切变区.(2)COL周围低臭氧浓度的气块源地也有两个,一是COL底部臭氧浓度相对较低的空气块主要来自急流轴右侧反气旋式风速切变区,以平流运动为主;二是COL前部及后部的空气块主要来自COL南侧低层暖区,以上升运动为主. | 李丹 卞建春 范秋君 | 2014 | 中国科学:地球科学2014，44，10： | 4 |
| 4 | 不同类型和强度的东亚切断低压过程中UTLS区域臭氧变化对比分析显示文摘利用ERA-Interim高分辨率臭氧资料和NCEP再分析资料,对比分析了不同类型(浅薄型和深厚型)、不同强度(针对深厚型)的东亚切断低压过程中伴随平流层空气入侵引起的上对流层-下平流层UTLS(Upper Troposphere-Low er Stratosphere)区域臭氧变化情况,结果表明:(1)深厚型和浅薄型切断低压过程中均出现了平流层臭氧入侵现象。在300 h Pa上,存在浅薄型切断低压引起的臭氧增量与深厚型切断低压相当的情况。在垂直分布上,深厚型个例臭氧浓度升高范围集中在对流层中上层至平流层下层区域,而浅薄个例中的臭氧浓度上升只集中发生在对流层中上层。(2)切断低压引起的UTLS区域臭氧浓度高值分布范围及臭氧含量大小与系统本身强度存在一定的联系。强度较强的深厚型切断低压过程中动力学对流层顶下降深度和入侵的臭氧浓度均远大于强度较弱的深厚型切断低压。(3)在选取11年臭氧平均值和11年当月臭氧平均值分别作为距平基准进行对比分析时发现,不同类型和强度的切断低压对比结果不受不同臭氧基准态选取的影响。 | 周天娇 陈丹 王咏青 郭栋 | 2018 | 高原气象2018，37，3： | 3 |
| 5 | The Impact of Cut-off Lows on Ozone in the Upper Troposphere and Lower Stratosphere over Changchun from Ozonesonde Observations显示文摘In situ measurements of the vertical structure of ozone were made in Changchun(43.53?N, 125.13?E), China, by the Institute of Atmosphere Physics, in the summers of 2010–13. Analysis of the 89 validated ozone profiles shows the variation of ozone concentration in the upper troposphere and lower stratosphere(UTLS) caused by cut-off lows(COLs) over Changchun. During the COL events, an increase of the ozone concentration and a lower height of the tropopause are observed.Backward simulations with a trajectory model show that the ozone-rich airmass brought by the COL is from Siberia. A case study proves that stratosphere–troposphere exchange(STE) occurs in the COL. The ozone-rich air mass transported from the stratosphere to the troposphere first becomes unstable, then loses its high ozone concentration. This process usually happens during the decay stage of COLs. In order to understand the influence of COLs on the ozone in the UTLS, statistical analysis of the ozone profiles within COLs, and other profiles, are employed. The results indicate that the ozone concentrations of the in-COL profiles are significantly higher than those of the other profiles between ±4 km around the tropopause. The COLs induce an increase in UTLS column ozone by 32% on average. Meanwhile, the COLs depress the lapse-rate tropopause(LRT)/dynamical tropopause height by 1.4/1.7 km and cause the atmosphere above the tropopause to be less stable. The influence of COLs is durable because the increased ozone concentration lasts at least one day after the COL has passed over Changchun. Furthermore, the relative coefficient between LRT height and lower stratosphere(LS) column ozone is-0.62,which implies a positive correlation between COL strength and LS ozone concentration. | Yushan SONG Daren LU Qian LI Jianchun BIAN Xue WU Dan LI | 2016 | Advances in Atmospheric Sciences2016，33，2： | 1 |
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