Aerosol Induced(气溶胶诱导)研究综述
Aerosol Induced 气溶胶诱导 - The seasonal analysis of meteorological factors including relative humidity (RH), precipitation, and boundary layer height (BLH) as well as regional fire activities expressed that the increased columnar AOD in spring was largely influenced by the hygroscopic growth of aerosol induced by the increased RH, the larger BLH causing the more effective transport and mixing of atmospheric particles to higher altitudes, and especially the intensive fire activities in the Southeast Asian region during the spring period, whereas the significantly increased surface PM2. [1]对相对湿度（RH）、降水量、边界层高度（BLH）等气象因素和区域火灾活动的季节分析表明，春季柱状AOD的增加主要受RH增加引起的气溶胶吸湿增长的影响。 , 较大的 BLH 导致大气颗粒更有效地向更高海拔输送和混合, 特别是春季期间东南亚地区的密集火灾活动, 而地表 PM2.5 显着增加。 [1]
aerosol induced heating
Proper incorporation of dust aerosol induced heating during breaks in models, is essential for simulation of intraseasonal variation inherent to Indian summer monsoon and thereby improving its prediction. [1] The estimated aerosol induced heating rate shows exponential decrease with height, but with high variability during each season. [2]在模型中断期间正确结合尘埃气溶胶引起的加热对于模拟印度夏季风固有的季节内变化并从而改进其预测至关重要。 [1] 估计的气溶胶诱导加热速率随高度呈指数下降，但在每个季节都有很大的变化。 [2]
aerosol induced snow 气溶胶致雪
Since surface albedo decides the sign and magnitude of aerosol direct radiative forcing, aerosol induced snow darkening significantly affects the direct radiative effects of aerosols. [1] Therefore, the present study highlights the heterogeneous response of aerosol induced snow albedo feedbacks over the Himalayan region and its impact on the snowpack and hydrology, which has further implications on the freshwater availability over the region. [2]由于地表反照率决定了气溶胶直接辐射强迫的符号和大小，气溶胶诱导的雪变暗显着影响气溶胶的直接辐射效应。 [1] 因此，本研究强调了喜马拉雅地区气溶胶诱导的雪反照率反馈的异质响应及其对积雪和水文的影响，这对该地区的淡水可用性有进一步的影响。 [2]