Arid
DOI10.1016/j.atmosenv.2020.117533
Aerosol absorption over the Aegean Sea under northern summer winds
Methymaki, Georgia1; Bossioli, Elissavet1; Kalogiros, John2; Kouvarakis, Giorgos3; Mihalopoulos, Nikolaos2,3; Nenes, Athanasios4,5; Tombrou, Maria1
通讯作者Methymaki, Georgia
来源期刊ATMOSPHERIC ENVIRONMENT
ISSN1352-2310
EISSN1873-2844
出版年2020
卷号231
英文摘要In this modelling study, the absorption influence on radiation, apart from scattering, is studied above the Aegean Sea (Eastern Mediterranean) under a typical warm 13-day period with northern winds, transporting polluted air masses. The simulated (WRF-Chem) forcing caused by the total absorption is estimated along with black carbon (BC), dust, and sea salt contributions, 1.3, 1.2, 0.1 and nearly zero W m(-2), accordingly. As dust and sea salt influence is negligible, the main focus is on BC. BC absorption reduces downward shortwave irradiance reaching the ground by up to 5.2 W m(-2) and the upward part by up to 1.7 W m(-2). The downward and the upward longwave irradiances are augmented by up to 2.3 and 1.2 W m(-2), accordingly. Even though the cloud formation is not favoured during the study period, BC absorption reduces overall the cloud water mixing ratio by 10% (semi-direct effect). However, during specific days and over limited cloudy areas, the semi-direct effect reduces low level clouds up to 20% while in case of higher clouds the reduction reaches up to similar to 29%. In order to examine the physical mechanisms below semi-direct effect, all modelled heating rates are analysed. Radiation direct absorption increases the air temperature with a rate up to 0.2 K day(-1), with an exception inside the surface layer, where unexpectedly longwave cooling prevails. The heating of the surface layer is mainly attributed to the advection process, as more heated air masses are transported over the Aegean Sea.
英文关键词Aerosol absorption Black carbon absorption WRF-Chem Direct effect Semi-direct effect heating rate Mediterranean Aerosol-radiation interaction
类型Article
语种英语
国家Greece ; Switzerland
收录类别SCI-E
WOS记录号WOS:000541247800014
WOS关键词OPTICAL-PROPERTIES ; AIR-POLLUTION ; HYGROSCOPIC PROPERTIES ; MEDITERRANEAN CLIMATE ; RADIATIVE-TRANSFER ; ABSORBING AEROSOL ; BOUNDARY-LAYER ; DESERT DUST ; MODEL ; SHORTWAVE
WOS类目Environmental Sciences ; Meteorology & Atmospheric Sciences
WOS研究方向Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/319432
作者单位1.Natl & Kapodistrian Univ Athens, Dept Phys, Athens 15772, Greece;
2.Natl Observ Athens, Inst Environm Res & Sustainable Dev, Athens 15236, Greece;
3.Univ Crete, Dept Chem, Iraklion 70013, Greece;
4.Ecole Polytech Fed Lausanne, Lab Atmospher Proc & Their Impacts, Sch Architecture Civil & Environm Engn, CH-1015 Lausanne, Switzerland;
5.Fdn Res & Technol Hellas, Inst Chem Engn Sci, Patras 26504, Greece
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GB/T 7714
Methymaki, Georgia,Bossioli, Elissavet,Kalogiros, John,et al. Aerosol absorption over the Aegean Sea under northern summer winds[J],2020,231.
APA Methymaki, Georgia.,Bossioli, Elissavet.,Kalogiros, John.,Kouvarakis, Giorgos.,Mihalopoulos, Nikolaos.,...&Tombrou, Maria.(2020).Aerosol absorption over the Aegean Sea under northern summer winds.ATMOSPHERIC ENVIRONMENT,231.
MLA Methymaki, Georgia,et al."Aerosol absorption over the Aegean Sea under northern summer winds".ATMOSPHERIC ENVIRONMENT 231(2020).
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