首页> 外文会议>Asian conference on remote sensing;ACRS >AEROSOL OPTICAL THICKNESS AND TOTAL OZONE COLUMN CHARACTERIZATION USING MICROTOPSⅡOZONEMETER IN MANILA, PHILIPPINES
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AEROSOL OPTICAL THICKNESS AND TOTAL OZONE COLUMN CHARACTERIZATION USING MICROTOPSⅡOZONEMETER IN MANILA, PHILIPPINES

机译:MICROTOPSⅡ臭氧仪在菲律宾马尼拉的气溶胶光学厚度和总臭氧柱特征

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Ground-based measurements of Total Ozone Column (TOC) and Aerosol Optical Thickness (AOT) at 1020 nm were done in Manila, Philippines (14.567° N, 120.980° E) using a MICROTOPSⅡozonemeter for the period of February to April 2014 at 30-minute intervals (0900-1200H, 1300-1600H, LT).For the study period, the lowest and highest TOC (at ±1σ) were 208.30±9.30 DU and 283.40±22.07 DU that occurred last March 18 and May 17, respectively. AOT had its lowest value of 0.117±0.045 last March 12 while the maximum was 0.335±0.11 last May 2. Kruskal-Wallis H statistics, a non-parametric analogue of ANOVA, revealed that the TOC values for the observation months are significantly different from each other (p = 0.0002). The same results were also obtained for AOT (p = 0). Mann-Whitney U Test, a non-parametric analogue of t-test, showed that there was a statistically significant difference in the values of TOC and AOT between the AM and PM observations with p-values of 0.032 and 0.001, respectively.The effects of relative humidity (RH) and surface temperature (ST) on AOT and TOC were analyzed. ST and RH play important roles in modulating aerosol and ozone behavior. For the study period, ST showed a moderately negative correlation with AOT (r= -0.4206) and a moderately positive correlation with TOC (r = +0.4922). RH had a strong positive correlation with AOT (r= +0.5431) but has very weak, negative correlation with TOC (r= -0.0339) which is not significant.
机译:使用MICROTOPSⅡ臭氧计在菲律宾马尼拉(14.567°N,120.980°E)于2014年2月至2014年4月30日在菲律宾马尼拉(14.567°N,120.980°E)进行了总臭氧柱(TOC)和气溶胶光学厚度(AOT)的地面测量。分钟间隔(0900-1200H,1300-1600H,LT)。在研究期间,最低和最高TOC(在±1σ时)分别为208.30±9.30 DU和283.40±22.07 DU,分别发生在去年3月18日和5月17日。 AOT在3月12日的最低值为0.117±0.045,而在5月2日的最大值为0.335±0.11。Kruskal-WallisH统计数据(ANOVA的非参数类似物)显示,观察月份的TOC值与彼此(p = 0.0002)。对于AOT也获得了相同的结果(p = 0)。曼氏惠特尼U检验(t检验的非参数类似物)显示AM和PM观察值之间的TOC和AOT值在统计学上有显着差异,p值分别为0.032和0.001。分析了AOT和TOC上的相对湿度(RH)和表面温度(ST)。 ST和RH在调节气溶胶和臭氧行为中起重要作用。在研究期间,ST与AOT呈中等程度的负相关(r = -0.4206),与TOC呈中等程度的正相关(r = +0.4922)。 RH与AOT呈极强的正相关(r = +0.5431),但与TOC呈极弱的负相关(r = -0.0339),这并不显着。

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