Assessment of the corrected CCN activation parameterizations in simulating shallow cumulus using large-eddy simulations DOI
Yuan Wang, Xiaoqi Xu, Chunsong Lu

и другие.

Atmospheric Research, Год журнала: 2024, Номер 315, С. 107881 - 107881

Опубликована: Дек. 22, 2024

Язык: Английский

The effects of aerosol on the growth of hydrometeors in deep convective clouds DOI
Xin Lin, Qian Chen,

Zeyong Zou

и другие.

Atmospheric Research, Год журнала: 2025, Номер unknown, С. 108088 - 108088

Опубликована: Март 1, 2025

Язык: Английский

Процитировано

0

Passive satellite hourly precipitation estimation over mainland China by combining cloud and meteorological parameters DOI

Sihang Xu,

Jiming Li, Jia Li

и другие.

Atmospheric Research, Год журнала: 2025, Номер unknown, С. 108112 - 108112

Опубликована: Апрель 1, 2025

Язык: Английский

Процитировано

0

Consistency Assessment of CORDEX Multi‐Domain Simulations Over the Tibetan Plateau Using REMO DOI
Ping Li, Xiaorui Niu,

Yanjin Mao

и другие.

International Journal of Climatology, Год журнала: 2025, Номер unknown

Опубликована: Апрель 29, 2025

ABSTRACT The Tibetan Plateau (TP), often referred to as the Water Tower of Asia and Third Pole, is undergoing rapid warming wetting, making it a key focus contemporary Earth System Science Research. Three Coordinated Regional Downscaling Experiment (CORDEX) domains: CORDEX‐EAS‐II, CORDEX‐CAS‐II CORDEX‐SAS‐II, overlap over TP, providing an opportunity assess sensitivity CORDEX simulations domain choice in this region. In study, we analyse similarities differences latest version Model (REMO) simulation across three domains at spatial resolution 25 km, focusing on climatology climate extremes. results show that has minimal impact REMO's extreme TP. Three‐dimensional indicators reveal primarily influences temporal evolution for temperature with effects magnitudes patterns. For precipitation simulations, more pronounced effect than variation or Additionally, significant seasonal biases are observed wet days, negative summer linked lower frequency 1–7 mm precipitation, while positive other seasons associated overestimation moderate‐to‐heavy rainfall frequencies.

Язык: Английский

Процитировано

0

Differential Impacts of Sub‐Daily Precipitation on Temperature Extremes Across China's Climatic Zones DOI Creative Commons
Chengqing Chen, Shanshan Wang, Zhiyang Wang

и другие.

Geophysical Research Letters, Год журнала: 2025, Номер 52(9)

Опубликована: Май 7, 2025

Abstract Precipitation events can effect temperature and modulate its response to climate change, yet the impact of sub‐daily precipitation on extremes in China has been understudied. This study therefore focuses daily maximum ( T max ) minimum min across China's climatic regions from 1952 2019. Results show that precipitation‐induced cooling effects through cloud evaporative cooling, particularly arid semi‐humid regions. In regions, enhances increased downward longwave radiation changes soil thermodynamics, while humid rainfall‐induced suppresses . Notably, warming trend during rainy weathers lacks statistical significance consistently warms more dry conditions. These findings reveal a saturation provide framework for understanding precipitation‐temperature interactions, with implications refining model assessing global warming.

Язык: Английский

Процитировано

0

Effect of Atmospheric Sulphate Aerosol on Precipitation over Central India: A Long-Term Evaluation Through Remote Sensing DOI
Anirban Middey,

Alexander J. Panjikkaran

Remote Sensing in Earth Systems Sciences, Год журнала: 2025, Номер unknown

Опубликована: Май 22, 2025

Язык: Английский

Процитировано

0

Distinct Microphysical Characteristics of Precipitating and Non‐Precipitating Parts of a Stratus Cloud From In Situ Aircraft Observations DOI
Jiefeng Li, Chuanfeng Zhao, Xiaobo Dong

и другие.

Journal of Geophysical Research Atmospheres, Год журнала: 2025, Номер 130(9)

Опубликована: Май 8, 2025

Abstract Cloud microphysical properties play a crucial role in stratus cloud behavior, with notable differences between precipitating and non‐precipitating parts. This study presents aircraft‐based observations on 8 May 2020 over coastal region China, to investigate the characteristics of liquid cloud. Significant aerosols number concentration ( N ), droplet c drizzle d ) are observed, lower concentrations part for all three. The effective radius r e droplets is smaller, while exhibit larger part. In part, decreases altitude, it remains constant due falling out. Aerosol size distribution analysis implies that precipitation mainly scavenges sizes smaller than 0.3 μm. particle distributions bimodal, broader spectrum especially layers. Additionally, drizzles contribute approximately 20% total water content 70% Our findings highlight distinct parts, playing critical microphysics formation.

Язык: Английский

Процитировано

0

The Impact of Air Pollution Control Programs (2014–2019) on the Vertical Structure of Precipitation in China DOI Creative Commons
Hongxia Zhu,

Renjun Zhou,

Hongwei Zhao

и другие.

Geophysical Research Letters, Год журнала: 2025, Номер 52(11)

Опубликована: Июнь 2, 2025

Abstract The impact of air pollution control programs on the vertical structure precipitation remains poorly understood. Using multiple data sources, we observed a yearly decrease in aerosol optical depth (AOD) southern China from 2014 to 2019, probably due these programs. In contrast, top height related rain onset (PTH 0 ), increased annually after accounting for thermodynamic variations. Further analyses revealed that, within mixed/lower atmospheric layers, growth precipitating particles (SlopeA/SlopeB) was significantly faster/slower compared subsequent years. correlation coefficients ( R ) between AOD and SlopeA PTH were 0.99 −0.94, respectively. As this study is based multi‐source observations, further research incorporating model simulations necessary elucidate mechanisms underlying emission reductions precipitation.

Язык: Английский

Процитировано

0

A review of aerosol-cloud interactions: Mechanisms, climate effects, and observation methods DOI
Tao Li, Yingying Yu, Xing Wang

и другие.

Atmospheric Research, Год журнала: 2025, Номер unknown, С. 108267 - 108267

Опубликована: Июнь 1, 2025

Язык: Английский

Процитировано

0

Combined effects of fine and coarse marine aerosol on vertical raindrop size distribution DOI Creative Commons
Fan Liu, Daniel Rosenfeld, Zengxin Pan

и другие.

npj Climate and Atmospheric Science, Год журнала: 2024, Номер 7(1)

Опубликована: Авг. 9, 2024

Abstract Climate models commonly overestimate warm rain frequency and underestimate its intensity over the ocean, primarily due to insufficient representation of aerosol effects. This pertains both fine aerosols (FA) coarse sea spray (CSA), where latter is mostly absent in models. Here, our observations show that adding CSA enhances vertical structure, contrast effect FA. The magnitude larger than opposite For with top heights 2–3 km, raindrop size, concentration, rate can be increased by factors 1.03, 1.47, 1.60, respectively. These CSA-induced changes are for thicker clouds, reaching a maximum 1.12, 1.85, 2.21, Therefore, combined FA effects should incorporated into climate accurately simulated precipitation microphysical processes.

Язык: Английский

Процитировано

2

Complex interplay of sulfate aerosols and meteorology conditions on precipitation and latent heat vertical structure DOI Creative Commons
Hongxia Zhu,

Shuping Yang,

Hongwei Zhao

и другие.

npj Climate and Atmospheric Science, Год журнала: 2024, Номер 7(1)

Опубликована: Авг. 21, 2024

An eight-year satellite observation dataset reveals that sulfate aerosols significantly influence the vertical structure of precipitation and latent heat (LH) in Beijing-Tianjin-Hebei (BTH) region during summer. In this period, prevalent combine with warm, humid southerly winds elevated convective available potential energy (CAPE), influencing dynamics. Under polluted conditions specific CAPE top temperature (PTT) ranges, particles experience accelerated growth within mixed-phase layer, delineated by −5 °C to 2 isotherms, compared pristine environments. This results a marked increase both intensity height at which maximum LH is released. Subsequent analysis hygroscopic aerosols, acting as cloud condensation nuclei (CCN), amplify collision-coalescence process mixed layer amid high water content, propelling rapid particle elevating PTT. warming effect surpasses cooling contribution from robust CAPE, culminating net elevation PTT under scenarios ones. Additionally, quantification sensitivity aerosol optical depth (AOD) unveils consistency between satellite-detected responses those predicted cloud-resolving model simulations. The study deduces role CCN either invigorating or diminishing contingent on water.

Язык: Английский

Процитировано

2