气候变化领域集成服务门户(CCPortal): Simulation of long-term direct aerosol radiative forcing over the arctic within the framework of the iAREA project

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DOI	10.1016/j.atmosenv.2020.117882
	Simulation of long-term direct aerosol radiative forcing over the arctic within the framework of the iAREA project
	Markowicz K.M.; Lisok J.; Xian P.
发表日期	2021
ISSN	1352-2310
卷号	244
英文摘要	This paper presents the climatology of aerosol optical properties and radiative forcing over the Arctic obtained within the framework of the iAREA (impact of absorbing aerosols on radiative forcing in the European Arctic) project. The presented data were obtained from the Navy Aerosol Analysis and Prediction System (NAAPS) and the Fu-Liou radiative transfer model. NAAPS was used to simulate particle concentration and aerosol optical depth (AOD) at 1 ° × 1 ° spatial resolution. Direct aerosol radiative forcing (ARF) was calculated for clear-sky and all-sky conditions based on NAAPS reanalysis (with AOD assimilation) and satellite observations of surface and cloud properties. Long-term data (2003–2015) from NAAPS show that anthropogenic and biogenic aerosol, as well as sea salt, make the most important contribution to total AOD (35 and 30%, respectively). However, smoke (15%) and mineral dust (20%) cannot be neglected, especially during spring and summer. Results of numerical simulations indicate mean shortwave (SW) ARF for the whole Arctic (>70.5oN) at the Earth's surface to be −4 W/m2 for clear-sky and −1.3 W/m2 for all-sky conditions, and at top of the atmosphere (TOA) −1.3 W/m2 and -0.4 W/m2, respectively. TOA ARF for anthropogenic and biogenic particles is only −0.1 W/m2 for clear-sky and almost zero for all-sky conditions. For smoke and dust particles, SW ARF is very similar for both Earth's surface and TOA, as well as for clear-sky and all-sky conditions. For sea salt, SW ARF is the same at the surface and at TOA: 0.6 W/m2 for clear-sky and −0.3 W/m2 for all-sky conditions, because of negligible solar absorption. Cloud cover reduces surface cooling (direct clear-sky SW ARF) by a factor of 40% and shifts TOA SW ARF towards positive values. © 2020 Elsevier Ltd
关键词	Absorbing aerosol Aerosol Aerosol optical depth Radiative forcing Single scattering albedo
语种	英语
scopus关键词	Atmospheric radiation; Dust; Optical properties; Radiative transfer; Smoke; Aerosol optical depths; Aerosol optical property; Direct aerosol radiative forcing; Particle concentrations; Radiative forcings; Radiative transfer model; Satellite observations; Top of the atmospheres; Aerosols; aerosol; clear sky; long-term change; optical depth; optical property; radiative forcing; radiative transfer; spatial resolution; aerosol; Article; climate change; controlled study; long term care; mineral dust; optical depth; particle size; priority journal; radiative forcing; sea ice; smoke; snow cover; solar radiation; surface property; surface stress; troposphere; uncertainty; water vapor
来源期刊	ATMOSPHERIC ENVIRONMENT
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/248883
作者单位	Institute of Geophysics, Faculty of Physics, University of Warsaw, Warsaw, 02-093, Poland; Naval Research Laboratory, Marine Meteorology Division, Monterey, United States
推荐引用方式 GB/T 7714	Markowicz K.M.,Lisok J.,Xian P.. Simulation of long-term direct aerosol radiative forcing over the arctic within the framework of the iAREA project[J],2021,244.
APA	Markowicz K.M.,Lisok J.,&Xian P..(2021).Simulation of long-term direct aerosol radiative forcing over the arctic within the framework of the iAREA project.ATMOSPHERIC ENVIRONMENT,244.
MLA	Markowicz K.M.,et al."Simulation of long-term direct aerosol radiative forcing over the arctic within the framework of the iAREA project".ATMOSPHERIC ENVIRONMENT 244(2021).