Modelling and Observation of Mineral Dust Optical Properties over Central Europe

• Autorzy: Chilinski M. T. , Markowicz K. M. , Zawadzka O. , Stachlewska I. S. , Kumala W. , Petelski T. , Makuch P. , Westphal D. L. , Zagajewski B.

Identyfikatory

DOI

10.1515/acgeo-2016-0069

• Języki publikacji: EN

Abstrakty

EN

This paper is focused on Saharan dust transport to Central Europe/ Poland; we compare properties of atmospheric Saharan dust using data from NAAPS, MACC, AERONET as well as observations obtained during HyMountEcos campaign in June 2012. Ten years of dust climatology shows that long-range transport of Saharan dust to Central Europe is mostly during spring and summer. HYSPLIT back-trajectories indicate airmass transport mainly in November, but it does not agree with modeled maxima of dust optical depth. NAAPS model shows maximum of dust optical depth (~0.04-0.05, 550 nm) in April-May, but the MACC modeled peak is broader (~0.04). During occurrence of mineral dust over Central-Europe for 14% (NAAPS) / 12% (MACC) of days dust optical depths are above 0.05 and during 4% (NAAPS) / 2.5% (MACC) of days dust optical depths exceed 0.1. The HyMountEcos campaign took place in June-July 2012 in the mountainous region of Karkonosze. The analysis includes remote sensing data from lidars, sunphotometers, and numerical simulations from NAAPS, MACC, DREAM8b models. Comparison of simulations with observations demonstrates the ability of models to reasonably reproduce aerosol vertical distributions and their temporal variability. However, significant differences between simulated and measured AODs were found. The best agreement was achieved for MACC model.

Słowa kluczowe

EN

aerosol; mineral dust; remote sensing; aerosol transport; MACC; NAAPS; DREAM

PL

aerozol; pył mineralny; teledetekcja; transport aerozolu

• Wydawca: Instytut Geofizyki PAN ; Springer
• Czasopismo: Acta Geophysica
• Rocznik: 2016
• Tom: Vol. 64, no. 6
• Strony: 2550--2590
• Opis fizyczny: Biibliogr. 95 poz.

Twórcy

autor

Chilinski M. T.

• Institute of Geophysics, Faculty of Physics, University of Warsaw, Warsaw, Poland
• College of Inter-Faculty Individual Studies in Mathematics and Natural Sciences, Warsaw, Poland

autor

Markowicz K. M.

• Institute of Geophysics, Faculty of Physics, University of Warsaw, Warsaw, Poland

autor

Zawadzka O.

• Institute of Geophysics, Faculty of Physics, University of Warsaw, Warsaw, Poland
• College of Inter-Faculty Individual Studies in Mathematics and Natural Sciences, Warsaw, Poland

autor

Stachlewska I. S.

• Institute of Geophysics, Faculty of Physics, University of Warsaw, Warsaw, Poland

autor

Kumala W.

• Institute of Geophysics, Faculty of Physics, University of Warsaw, Warsaw, Poland

autor

Petelski T.

• Institute of Oceanology, Polish Academy of Sciences, Sopot, Poland

autor

Makuch P.

• Institute of Oceanology, Polish Academy of Sciences, Sopot, Poland

autor

Westphal D. L.

• Marine Meteorology Division, Naval Research Laboratory, Monterey, CA, USA

autor

Zagajewski B.

• Department of Geoinformatics and Remote Sensing, Faculty of Geography and Regional Studies, University of Warsaw, Warsaw, Poland

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Uwagi

Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę (zadania 2017)