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Relationships between ten-year trends of tropospheric ozone and temperature over Taiwan

机译:台湾对流层臭氧十年趋势与温度的关系

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摘要

The analyses of ten-year ozonesonde observations from 1993 till 2002, over Taipei, Taiwan show influences of climate change. Despite huge increases in its precursor emissions in this region, there were little variations in tropospheric ozone. Results indicate a warmer troposphere, a statistically insignificant rising tropopause, 79 ±206 m per decade, and decreasing tropopause temperature at -1.0±0.89 K per decade. The derived mean tropospheric ozone is 40.58 ± 10.99 DU, and has a statistically insignificant small trend of -0.78 ±1.7 DU per decade. The derived ten-year vertical trends of temperature and ozone are inversely correlated with each other from the middle troposphere up to the lower stratosphere. The averaged monthly vertical temperature trends show a generally warmer middle troposphere. The tropospheric ozone monthly trend has small increases only in the lower troposphere during winter and spring. Strong decreases occur in summer, from the surface up into the stratosphere. For ozone variation, results suggest that influences of climate forcing are stronger than those from precursor increases. More frequent and/or intense convection in summer and other climate-induced effects may contribute to the less than expected ozone observed in the troposphere.
机译:对台湾台北市从1993年至2002年的十年探空仪观测资料进行的分析显示了气候变化的影响。尽管该区域的前体排放量大量增加,但对流层臭氧变化不大。结果表明对流层变暖,对流层顶上升在统计学上不显着,每十年为79±206 m,对流层顶温度下降为每十年-1.0±0.89K。推算出的平均对流层臭氧为40.58±10.99 DU,每十年有-0.78±1.7 DU的统计上无统计学意义的小趋势。从对流层中层到平流层下层,得出的十年温度和臭氧的垂直趋势相互负相关。平均每月垂直温度趋势表明对流层中部普遍变暖。对流层臭氧的月度趋势仅在冬季和春季在对流层较低处增加很小。在夏季,从地表到平流层都有明显的下降。对于臭氧变化,结果表明,气候强迫的影响要强于前兆增加的影响。夏季更频繁和/或更强烈的对流以及其他气候引起的影响可能导致对流层中观测到的臭氧少于预期。

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