Pregled bibliografske jedinice broj: 1031870
Convective dust storms during Saharan dust outbreak on Northern Adriatic
Convective dust storms during Saharan dust outbreak on Northern Adriatic // European Conference on Severe Stroms
Kraków, Poljska, 2019. (poster, međunarodna recenzija, neobjavljeni rad, ostalo)
CROSBI ID: 1031870 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Convective dust storms during Saharan dust outbreak on Northern Adriatic
Autori
Mifka, Boris ; Telišman Prtenjak, Maja
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, neobjavljeni rad, ostalo
Skup
European Conference on Severe Stroms
Mjesto i datum
Kraków, Poljska, 04.11.2019. - 08.11.2019
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Pješčane kovektivne oluje, WRF-Chem
(Convective dust storms, WRF-Chem)
Sažetak
Airborne mineral dust affects the climate by modifying radiation budget, formation of clouds and marine bio-geochemical cycles. It’s most abundant global source, Saharan desert, has strong influence on the Mediterranean countries. The increase of PM10 hourly values due to Saharan dust outbreak was observed at several ground based air quality stations located on Italian and Croatian Adriatic coast in September 2015. According to previous studies, two major mechanisms contribute to dust emissions ; the Nocturnal Low Level Jet (NLLJ) breakdown and convective dust storms, Haboobs. WRF-Chem model was applied to simulate the dust emission, transport and deposition, and two major sources of dust in Algeria and Tunisia were detected during the episode. The temporal evolution of spatially averaged dust emission at sources locations show strong morning peaks characteristic for NLLJ breakdowns. However, using North African Sandstorm Survey (NASCube) method, the Haboob development is observed and according to Aerosol Optical Depth (AOD) product possibly contributing to Algerian dust source emission. Although the model’s coarse resolution does not allow the grid resolved simulation of convective processes, the model shows good agreement with AOD measured at 8 African and European AERONET stations and with PM10 measured at 10 Italian and Croatian air quality stations.
Izvorni jezik
Engleski
Znanstvena područja
Geofizika
POVEZANOST RADA
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb,
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