A comprehensive study about the in-cloud processing of nitrate through coupled measurements of individual cloud residuals and cloud water
oleh: G. Zhang, G. Zhang, G. Zhang, X. Hu, X. Hu, X. Hu, W. Sun, W. Sun, W. Sun, Y. Yang, Y. Yang, Z. Guo, Z. Guo, Z. Guo, Y. Fu, Y. Fu, H. Wang, S. Zhou, L. Li, M. Tang, M. Tang, M. Tang, Z. Shi, D. Chen, X. Bi, X. Bi, X. Bi, X. Wang, X. Wang, X. Wang
| Format: | Article |
|---|---|
| Diterbitkan: | Copernicus Publications 2022-07-01 |
Deskripsi
<p>While the formation and evolution of nitrate in airborne particles are extensively investigated, little is known about the processing of nitrate in clouds. Here we present a detailed investigation on the in-cloud formation of nitrate, based on the size-resolved mixing state of nitrate in the individual cloud residual and cloud-free particles obtained by single particle mass spectrometry, and also the mass concentrations of nitrate in the cloud water and PM<span class="inline-formula"><sub>2.5</sub></span> at a mountain site (1690 m a.s.l. – above sea level) in southern China. The results show a significant enhancement of nitrate mass fraction and relative intensity of nitrate in the cloud water and the cloud residual particles, respectively, reflecting a critical role of in-cloud processing in the formation of nitrate. We first exclude the gas-phase scavenging of HNO<span class="inline-formula"><sub>3</sub></span> and the facilitated activation of nitrate-containing particles as the major contribution for the enhanced nitrate, according to the size distribution of nitrate in individual particles. Based on regression analysis and theoretical calculations, we then highlight the role of N<span class="inline-formula"><sub>2</sub></span>O<span class="inline-formula"><sub>5</sub></span> hydrolysis in the in-cloud formation of nitrate, even during the daytime, attributed to the diminished light in clouds. Nitrate is highly related (<span class="inline-formula"><i>R</i><sup>2</sup>=</span> <span class="inline-formula">∼</span> 0.6) to the variations in [NO<span class="inline-formula"><sub><i>x</i></sub></span>][O<span class="inline-formula"><sub>3</sub></span>], temperature, and droplet surface area in clouds. Accounting for droplet surface area greatly enhances the predictability of the observed nitrate, compared with using [NO<span class="inline-formula"><sub><i>x</i></sub></span>][O<span class="inline-formula"><sub>3</sub></span>] and temperature. The substantial contribution of N<span class="inline-formula"><sub>2</sub></span>O<span class="inline-formula"><sub>5</sub></span> hydrolysis to nitrate in clouds with diminished light during the daytime can be reproduced by a multiphase chemical box model. Assuming a photolysis rate at 30 % of the default setting, the overall contribution of N<span class="inline-formula"><sub>2</sub></span>O<span class="inline-formula"><sub>5</sub></span> hydrolysis pathway to nitrate formation increases by <span class="inline-formula">∼</span> 20 % in clouds. Given that N<span class="inline-formula"><sub>2</sub></span>O<span class="inline-formula"><sub>5</sub></span> hydrolysis acts as a major sink of NO<span class="inline-formula"><sub><i>x</i></sub></span> in the atmosphere, further model updates would improve our understanding about the processes contributing to nitrate production in cloud and the cycling of odd nitrogen.</p>