Type‐Dependent Impact of Aerosols on Precipitation Associated With Deep Convective Cloud Over East Asia

Geophysical Research Letters

et al. 2023

Section: Methodsmentioning

confidence: 99%

Vertical Dependency of Aerosol Impacts on Local Scale Convective Precipitation

Sun

Wang

Geophysical Research Letters

et al. 2023

“…The uncertainty of aerosol effects on cloud and precipitation is highly dependent on the meteorological conditions (Han et al., 2022; Z. Li et al., 2011; Stevens & Feingold, 2009). Previous studies (Bai et al., 2018; Filioglou et al., 2019; X. Ma et al., 2018; Matsui et al., 2004) used the lower‐tropospheric static stability, defined as the potential temperature difference between the sea level and 700 hPa, to describe the thermodynamic condition in the study of aerosol effect on the cloud.…”

Section: Methodsmentioning

confidence: 99%

“…The uncertainty of aerosol effects on cloud and precipitation is highly dependent on the meteorological conditions (Han et al, 2022;Z. Li et al, 2011;Stevens & Feingold, 2009).…”

Section: Meteorologymentioning

confidence: 99%

Spatial Heterogeneity of Aerosol Effect on Liquid Cloud Microphysical Properties in the Warm Season Over Tibetan Plateau

Yuan

et al. 2023

JGR Atmospheres

The effect of aerosol on liquid cloud microphysical properties over the Tibetan Plateau (TP) during the warm season is investigated by using aerosol index (AI) and cloud property parameters data. Distinct differences in aerosol effect on liquid cloud microphysical properties have been found between the northern Tibetan Plateau (NTP) and southernTibetan Plateau (STP). The composite liquid cloud droplet effective radius liquid cloud droplet effective radius (LREF) anomalies for positive AI events are positive in the NTP and negative in the STP. In both NTP and STP, when the AI anomalies are positive, the LREF anomalies are also positive, which suggests that the increased aerosol loading reduces the solar radiation reaching the ground and thus enhances the atmospheric stability, which reduces the cloud base height and makes the liquid cloud area thicker, which gives cloud droplets more space to grow by collision‐coalescence. This indicates that the aerosol radiative effect is not likely the reason causing the distinct differences of aerosol effects on liquid cloud properties between NTP and STP. Further analysis shows that in the STP, the LREF first increases and then decreases with the increase of AI, while in the NTP, the LREF always increases with the increase of AI, suggesting a spatial difference in aerosol microphysical effect. In the STP, the influence of aerosol on liquid clouds is mainly dependent on liquid water path and convective available potential energy, while in the NTP, the influence of aerosol on liquid cloud is more likely related to large aerosol particles.

“…The uncertainty of aerosol effects on cloud and precipitation is highly dependent on the meteorological conditions (Li et al, 2011;Han et al, 2022;Stevens and Feingold, 2009). Previous studies (Bai et al, 2018;Filioglou et al, 2019;Ma et al, 2018;Matsui et al, 2004) used the lower-tropospheric static stability (LTS), defined as the potential temperature difference between the sea level and 700 hPa, to describe the thermodynamic condition in the study of aerosol effect on the cloud.…”

Section: Meteorologymentioning

confidence: 99%

Spatial heterogeneity of aerosol effect on liquid cloud microphysical properties in the warm season over Tibetan Plateau

Yuan

et al. 2022

Preprint

The effect of aerosol on liquid cloud microphysical properties over the Tibetan Plateau during the warm season is investigated by employing aerosol index and cloud property parameters. Distinct differences in aerosol effect on liquid cloud microphysical properties have been found between the northern TP (NTP) and southern TP (STP). The composite liquid cloud droplet effective radius (LREF) anomalies for positive aerosol index (AI) events are positive in the NTP and negative in the STP.In both NTP and STP, when the AI anomalies are positive, the LREF anomalies are also positive, which suggests that the increased aerosol loading reduces the solar radiation reaching the ground and thus enhances the atmospheric stability, making cloud droplets not conducive to break up. This indicates that the aerosol radiative effect is not likely the reason causing the distinct differences of aerosol effects on liquid cloud properties between NTP and STP. Further analysis shows that in the STP, the LREF first increases and then decreases with the increase of AI, while in the NTP, the LREF always increases with the increase of AI, suggesting a spatial difference in aerosol microphysical effect. In the STP, the influence of aerosol on liquid clouds is mainly dependent on liquid water path (LWP) and convective available potential energy (CAPE), while in the NTP, the influence of aerosol on liquid cloud is more likely related to large aerosol particles.