The different effects on the climate in China area between the model with variable and stable total ozone are analyzed.
以中国地区为例，对比模拟了考虑臭氧随季节、纬度变化和模式原有的固定臭氧值对气候的不同影响。
The total ozone amount at the area of Zhongshan Station has been decreasing during recent 7 years, which is similar to the trend of the global ozone variation.
近7年来，中山站地区的大气臭氧总量有减少趋势，与全球大气臭氧总量变化趋势相同。
Model simulations indicate that the surface UVI at Mt. Waliguan will increase 5% from 2000 to 2010, 16% from 2000 to 2030 if the total ozone decreases by 0.34%yr-1.
模式模拟结果表明，若瓦里关臭氧总量在2000年的基础上以0.34%的年递减率变化，则到2010,uvi将上升5%左右，到2030年，UVI将上升16%左右。
The TOMS total ozone data observed by satellite has been used to the regional climate modeling considering the variation of the total ozone amount with season and latitude.
将卫星观测的TOMS臭氧总量资料应用于区域气候模拟中，在不同纬度的地区采用随季节变化的臭氧总量。
The calculation results show that the ultraviolet radiation received at the ground is more sensitive to changes in atmospheric turbidity than changes in the total ozone amount.
最后给出了北京地区地面太阳紫外总辐射的变化趋势，计算结果表明，地面太阳紫外总辐射对大气浑浊度的变化比对大气臭氧总量的变化敏感得多。
Since the discovery of Antarctic springtime ozone hole in 1985, there has been much international attention focused on the possible consequences of significant decreases of total ozone.
自1985年发现南极春季臭氧洞以来，对于臭氧大幅度减少所引起的可能后果与危害引起了国际关注。
There are close relations between the losses of total ozone in spring and summer and the uplift of the second tropopause height in summer over the Qinghai-Xizang Plateau in recent 30 years.
近30年春、夏季高原臭氧总量亏损与夏季高原第二对流层顶高度的抬升存在着密切关系。
Analysis of the observational data, the TOMS total ozone, and NCEP circulation, shows that the atmospheric ozone amount experienced a high-low-high variation with low-high-low tropopause altitude.
分析大气监测资料、TOMS臭氧总量资料和NCEP大气环流资料表明，大气臭氧总量随着对流层顶的低一高一低变化呈高一低一高的变化过程。
The relationship between the total amount of ozone and the rainfall in Kunming area has been studied using factor analysis and spectrum analysis.
利用因子分析和谱分析方法，探讨昆明地区臭氧总量变化与降水的关系。
The total amount of ozone overheaded in late winter and early spring at Antarctica has decreased by about 30-40 per cent during past decade to form an "ozone hole".
南极臭氧总量在晚冬和早春减少了30—40％，形成一个“臭氧洞”。本文概述了一些作者对这一观测事实给出的解释，以期使读者对此问题有一个全面的认识。
The total amount of ozone overheaded in late winter and early spring at Antarctica has decreased by about 30-40 per cent during past decade to form an "ozone hole".
南极臭氧总量在晚冬和早春减少了30—40％，形成一个“臭氧洞”。本文概述了一些作者对这一观测事实给出的解释，以期使读者对此问题有一个全面的认识。
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