干旱区生态环境知识资源中心(Arid): Two-dimensional mineral dust radiative effect calculations from CALIPSO observations over Europe

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DOI	10.5194/acp-19-13157-2019
	Two-dimensional mineral dust radiative effect calculations from CALIPSO observations over Europe
	Jose Granados-Munoz, Maria 1,2,3; Sicard, Michael 1,4; Papagiannopoulos, Nikolaos 1,5; Barragan, Ruben 1,4; Antonio Bravo-Aranda, Juan 2,3; Nicolae, Doina 6
通讯作者	Jose Granados-Munoz, Maria
来源期刊	ATMOSPHERIC CHEMISTRY AND PHYSICS
ISSN	1680-7316
EISSN	1680-7324
出版年	2019
卷号	19 期号:20 页码:13157-13173
英文摘要	A demonstration study to examine the feasibility of retrieving dust radiative effects based on combined satellite data from MODIS (Moderate Resolution Imaging Spectroradiometer), CERES (Clouds and the Earth's Radiant Energy System) and CALIOP (Cloud-Aerosol Lidar with Orthogonal Polarization) lidar vertical profiles along their orbit is presented. The GAME (Global Atmospheric Model) radiative transfer model is used to estimate the shortwave and longwave dust radiative effects below the CALIPSO (Cloud-Aerosol Lidar and Infrared Pathfinder Satellite) orbit assuming an aerosol parameterization based on the CALIOP vertical distribution at a horizontal resolution of 5 km and additional AERONET (Aerosol Robotic Network) data. Two study cases are analyzed: a strong long-range transport mineral dust event (aerosol optical depth, AOD, of 0.52) that originated in the Sahara Desert and reached the United Kingdom and a weaker event (AOD = 0.16) that affected eastern Europe. The radiative fluxes obtained are first validated in terms of radiative efficiency at a single point with space-time colocated lidar ground-based measurements from EARLINET (European Aerosol Research Lidar Network) stations below the orbit. The methodology is then applied to the full orbit. The strong dependence of the radiative effects on the aerosol load (and to a lesser extent on the surface albedo) highlights the need for accurate AOD measurements for radiative studies. The calculated dust radiative effects and heating rates below the orbits are in good agreement with previous studies of mineral dust, with the radiative efficiency obtained at the surface ranging between -80.3 and -63.0 W m(-2) for lower dust concentration event and -119.1 and -79.3W m(-2) for the strong event. Thus, results demonstrate the validity of the method presented here to retrieve 2-D accurate radiative properties with large spatial and temporal coverage.
类型	Article
语种	英语
国家	Spain ; Italy ; Romania
开放获取类型	Green Submitted, Green Published, gold
收录类别	SCI-E
WOS记录号	WOS:000492830900002
WOS关键词	AEROSOL OPTICAL DEPTH ; ENERGY SYSTEM CERES ; SAHARAN DUST ; RAMAN LIDAR ; DESERT DUST ; ALGORITHM ; SHORTWAVE ; SATELLITE ; LONGWAVE ; PRODUCTS
WOS类目	Environmental Sciences ; Meteorology & Atmospheric Sciences
WOS研究方向	Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
EI主题词	2019-10-24
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/310345
作者单位	1.Univ Politecn Cataluna, Remote Sensing Lab, CommSensLab, ES-08034 Barcelona, Spain; 2.Andalusian Interuniv Inst Earth Syst Res IISTA CE, Avd Mediterraneo, Granada 18006, Spain; 3.Univ Granada, Dept Appl Phys, Fuentenueva S-N, E-18071 Granada, Spain; 4.Univ Politecn Cataluna, CTE CRAE IEEC, ES-08034 Barcelona, Spain; 5.CNR IMAA, I-85050 Tito, Italy; 6.Natl Inst R&D Optoelect INOE, Magurele 77125, Romania
推荐引用方式 GB/T 7714	Jose Granados-Munoz, Maria,Sicard, Michael,Papagiannopoulos, Nikolaos,et al. Two-dimensional mineral dust radiative effect calculations from CALIPSO observations over Europe[J],2019,19(20):13157-13173.
APA	Jose Granados-Munoz, Maria,Sicard, Michael,Papagiannopoulos, Nikolaos,Barragan, Ruben,Antonio Bravo-Aranda, Juan,&Nicolae, Doina.(2019).Two-dimensional mineral dust radiative effect calculations from CALIPSO observations over Europe.ATMOSPHERIC CHEMISTRY AND PHYSICS,19(20),13157-13173.
MLA	Jose Granados-Munoz, Maria,et al."Two-dimensional mineral dust radiative effect calculations from CALIPSO observations over Europe".ATMOSPHERIC CHEMISTRY AND PHYSICS 19.20(2019):13157-13173.