کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4442327 1311146 2008 25 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Relative humidity dependence of aerosol optical properties and direct radiative forcing in the surface boundary layer at Xinken in Pearl River Delta of China: An observation based numerical study
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات علم هواشناسی
پیش نمایش صفحه اول مقاله
Relative humidity dependence of aerosol optical properties and direct radiative forcing in the surface boundary layer at Xinken in Pearl River Delta of China: An observation based numerical study
چکیده انگلیسی

In a numerical study, influences of relative humidity (RH) on aerosol optical properties and direct radiative forcing in the surface boundary layer at Xinken (XK) in Pearl River Delta of China are investigated based on the observed particle hygroscopic growth (fg(Dp,RH)fg(Dp,RH)) and the relevant aerosol physical and chemical properties. The model is validated by comparing the simulated ambient extinction coefficients with those measured by a Raman LIDAR. At 550 nm, the scattering coefficient increases with a factor of 1.54 and 2.31 at a RH increase from 30% to 80% and 90%, respectively. This ratio is mainly controlled by fgfg, and generally increases with increasing wavelength and decreases with increasing particle effective diameter. From RH 30% to 90%, the average single scattering albedo (ω0ω0) changes from 0.77 to 0.88, 0.91 to 0.97, and 0.86 to 0.94 for internal, respectively, external mixtures, and the retrieved mixing state of the elemental carbon (EC) at XK. The assumption that the absorption coefficient does not change upon humidification alone can introduce an overestimation of ω0ω0 of 0.02 (∼5%∼5%) at RH 90% for an internal mixture. However, accounting for the EC mixing state at XK, this error is only about 0.3%. The mean upscatter fraction (β¯) is evaluated as 0.233 at RH 30% with a 30% decrease to 0.191 at RH 90%. The estimation of aerosol direct radiative forcing (ΔFRΔFR) in the surface boundary layer at XK strongly depends on RH and the EC mixing state. The critical ω0ω0 at XK is estimated to be about 0.77–0.80 at 550 nm. Assuming an internal or coated mixture of EC, no pronounced ΔFRΔFR is observed when RH<60%RH<60%, whereas a cooling effect arises while RH>60%RH>60%. Under the actual EC mixing conditions at XK, the effect of ΔFRΔFR is cooling. Over 40% of this cooling effect is contributed by water at RH 80% and ΔFRΔFR at RH 90% exceeds that at RH 30% by about a factor of 2.7.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Atmospheric Environment - Volume 42, Issue 25, August 2008, Pages 6373–6397
نویسندگان
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