• Then, the total surface radiative forcing was simulated.

    然后,进行地面总辐射强迫的模拟试验。

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  • Radiative forcing will be affected deeply by the change of single scattering albedo of dust aerosol.

    辐射强迫数值对矿物尘气溶胶单次散射反照率的变化较敏感。

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  • The annual mean negative net cloud radiative forcing in the eastern China is obviously larger than that in the Indian region.

    年平均的负的短波云辐射强迫在中国东部地区明显要大于在印度季风区。

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  • Based on the analysis, the increasing of ozone in troposphere can lead to almost positive clear sky radiative forcing at top of atmosphere.

    通过对比模拟发现:对流层中臭氧的增加基本使大气顶晴空辐射强迫为正;

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  • The geographical and temporal distribution pattern of aerosol radiative forcing is generally consistent with that of aerosol optical depth.

    气溶胶辐射强迫的分布与其光学厚度的分布基本一致。

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  • The radiative forcing due to human activity in some areas can be comparable in magnitude with the forcing caused by greenhouse gases, such as CO2 etc.

    某些地区人为气溶胶的强迫在量值上可与CO2等温室气体引起的强迫相比拟。

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  • Aerosol has much influence on the earth-atmosphere climate system through its impact on direct and indirect radiative forcing. It also plays a crucial role in regional air pollution problems.

    大气气溶胶质粒通过直接辐射强迫和间接辐射强迫两种方式影响着地球气候系统,同时,它在区域环境空气质量问题上也扮演重要角色。

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  • By the further analysis to the climate responses, the simulation results show the gradually increasing uncertainties from sulfate contents to radiative forcing and surface temperature response.

    通过对气候响应的进一步分析发现:模拟结果显示了从硫酸盐含量到辐射强迫和地表温度响应逐渐加大的不确定性。

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  • The effects of ozone in troposphere on climate factors such as radiative forcing, surface temperature air temperature, have been discussed by coupling regional climate model and chemical model.

    利用耦合的区域气候模式和大气化学模式模拟对流层臭氧的产生、分布和对辐射传输、地表温度、气温等的影响。

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  • The effects of ozone in troposphere on climate factors such as radiative forcing, surface temperature air temperature, have been discussed by coupling regional climate model and chemical model.

    利用耦合的区域气候模式和大气化学模式模拟对流层臭氧的产生、分布和对辐射传输、地表温度、气温等的影响。

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