Climate Change Data Portal
DOI | 10.5194/acp-21-2765-2021 |
A-Train estimates of the sensitivity of the cloud-to-rainwater ratio to cloud size, relative humidity, and aerosols | |
M. Smalley K.; D. Rapp A. | |
发表日期 | 2021 |
ISSN | 1680-7316 |
起始页码 | 2765 |
结束页码 | 2779 |
卷号 | 21期号:4 |
英文摘要 | Precipitation efficiency has been found to play an important role in constraining the sensitivity of the climate through its role in controlling cloud cover, yet its controls are not fully understood. Here we use CloudSat observations to identify individual contiguous shallow cumulus cloud objects and compute the ratio of cloud water path to rainwater (WRR) path as a proxy for warm-rain efficiency. Cloud objects are then conditionally sampled by cloud-top height, relative humidity, and aerosol optical depth (AOD) to analyze changes in WRR as a function of cloud size (extent). For a fixed cloud-top height, WRR increases with extent and environmental humidity following a double power-law distribution, as a function of extent. Similarly, WRR increases, holding average relative humidity at or below 850 mb constant. There is little relationship between WRR and AOD when conditioned by cloud-top height, suggesting that, once rain drop formation begins, aerosols may not be as important for WRR as cloud size and depth. Consistent with prior studies, results show an increase in WRR with sea-surface temperature. However, for a given depth and SST, WRR is also dependent on cloud size and becomes larger as cloud size increases. Given that larger objects become more frequent with increasing SST, these results imply that increasing precipitation efficiencies with SST are due not only to deeper clouds with greater cloud water contents but also to the propensity for larger clouds which may have more protected updrafts. © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. |
语种 | 英语 |
scopus关键词 | aerosol; CloudSat; cumulus; optical depth; power law distribution; rainwater; relative humidity; sea surface temperature; sensitivity analysis |
来源期刊 | ATMOSPHERIC CHEMISTRY AND PHYSICS |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/247119 |
作者单位 | Department of Atmospheric Sciences, Texas AandM University, College Station, TX, United States |
推荐引用方式 GB/T 7714 | M. Smalley K.,D. Rapp A.. A-Train estimates of the sensitivity of the cloud-to-rainwater ratio to cloud size, relative humidity, and aerosols[J],2021,21(4). |
APA | M. Smalley K.,&D. Rapp A..(2021).A-Train estimates of the sensitivity of the cloud-to-rainwater ratio to cloud size, relative humidity, and aerosols.ATMOSPHERIC CHEMISTRY AND PHYSICS,21(4). |
MLA | M. Smalley K.,et al."A-Train estimates of the sensitivity of the cloud-to-rainwater ratio to cloud size, relative humidity, and aerosols".ATMOSPHERIC CHEMISTRY AND PHYSICS 21.4(2021). |
条目包含的文件 | 条目无相关文件。 |
个性服务 |
推荐该条目 |
保存到收藏夹 |
导出为Endnote文件 |
谷歌学术 |
谷歌学术中相似的文章 |
[M. Smalley K.]的文章 |
[D. Rapp A.]的文章 |
百度学术 |
百度学术中相似的文章 |
[M. Smalley K.]的文章 |
[D. Rapp A.]的文章 |
必应学术 |
必应学术中相似的文章 |
[M. Smalley K.]的文章 |
[D. Rapp A.]的文章 |
相关权益政策 |
暂无数据 |
收藏/分享 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。