Suppr超能文献

通过气象分析量化全球尘卷风的发生情况。

Quantifying global dust devil occurrence from meteorological analyses.

作者信息

Jemmett-Smith Bradley C, Marsham John H, Knippertz Peter, Gilkeson Carl A

机构信息

Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds Leeds, UK.

Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds Leeds, UK ; National Centre for Atmospheric Science Leeds, UK.

出版信息

Geophys Res Lett. 2015 Feb 28;42(4):1275-1282. doi: 10.1002/2015GL063078. Epub 2015 Feb 26.

Abstract

UNLABELLED

Dust devils and nonrotating dusty plumes are effective uplift mechanisms for fine particles, but their contribution to the global dust budget is uncertain. By applying known bulk thermodynamic criteria to European Centre for Medium-Range Weather Forecasts (ECMWF) operational analyses, we provide the first global hourly climatology of potential dust devil and dusty plume (PDDP) occurrence. In agreement with observations, activity is highest from late morning into the afternoon. Combining PDDP frequencies with dust source maps and typical emission values gives the best estimate of global contributions of 3.4% (uncertainty 0.9-31%), 1 order of magnitude lower than the only estimate previously published. Total global hours of dust uplift by dry convection are ∼0.002% of the dust-lifting winds resolved by ECMWF, consistent with dry convection making a small contribution to global uplift. Reducing uncertainty requires better knowledge of factors controlling PDDP occurrence, source regions, and dust fluxes induced by dry convection.

KEY POINTS

Global potential dust devil occurrence quantified from meteorological analyses Climatology shows realistic diurnal cycle and geographical distribution Best estimate of global contribution of 3.4% is 10 times smaller than the previous estimate.

摘要

未标注

尘卷风和非旋转沙尘羽流是细颗粒物的有效抬升机制,但其对全球沙尘收支的贡献尚不确定。通过将已知的整体热力学标准应用于欧洲中期天气预报中心(ECMWF)的业务分析,我们首次给出了全球每小时潜在尘卷风和沙尘羽流(PDDP)出现情况的气候学数据。与观测结果一致,其活动在上午晚些时候到下午最为频繁。将PDDP频率与沙尘源地图及典型排放值相结合,得出全球贡献的最佳估计值为3.4%(不确定性为0.9 - 31%),比之前唯一发表的估计值低1个数量级。全球因干对流导致的沙尘抬升总时长约占ECMWF解析出的沙尘起扬风时长的0.002%,这与干对流对全球沙尘抬升贡献较小相一致。减少不确定性需要更好地了解控制PDDP出现的因素、源区以及干对流引发的沙尘通量。

关键点

通过气象分析量化全球潜在尘卷风出现情况

气候学显示出符合实际的日循环和地理分布

全球贡献的最佳估计值3.4%比之前的估计值小10倍。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6c4f/4670712/6ddf65225c78/grl0042-1275-f1.jpg

文献检索

告别复杂PubMed语法,用中文像聊天一样搜索,搜遍4000万医学文献。AI智能推荐,让科研检索更轻松。

立即免费搜索

文件翻译

保留排版,准确专业,支持PDF/Word/PPT等文件格式,支持 12+语言互译。

免费翻译文档

深度研究

AI帮你快速写综述,25分钟生成高质量综述,智能提取关键信息,辅助科研写作。

立即免费体验