Anna Rozwadowska

ORCID: 0000-0002-4450-6551
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About
Contact & Profiles
Research Areas
  • Atmospheric chemistry and aerosols
  • Atmospheric aerosols and clouds
  • Atmospheric Ozone and Climate
  • Atmospheric and Environmental Gas Dynamics
  • Solar Radiation and Photovoltaics
  • Climate variability and models
  • Arctic and Antarctic ice dynamics
  • Cryospheric studies and observations
  • Geology and Paleoclimatology Research
  • Maritime Transport Emissions and Efficiency
  • Aeolian processes and effects
  • Climate change and permafrost
  • Marine and environmental studies
  • Conservation, Biodiversity, and Resource Management
  • Radioactive contamination and transfer
  • Wind Energy Research and Development
  • Aerospace Engineering and Energy Systems
  • Solar and Space Plasma Dynamics
  • Impact of Light on Environment and Health
  • Per- and polyfluoroalkyl substances research
  • Peatlands and Wetlands Ecology
  • Air Quality and Health Impacts
  • Environmental Conservation and Management
  • Radioactivity and Radon Measurements
  • Economic and Environmental Valuation

Instytut Oceanologii Polskiej Akademii Nauk
2010-2024

Polish Academy of Sciences
2013-2024

Goddard Space Flight Center
2002

National Academy of Sciences
2000

National Academies of Sciences, Engineering, and Medicine
2000

Abstract. In this paper, spectra of aerosol optical thickness from the AERONET (AErosol RObotic NETwork) station at Hornsund in southern part Spitsbergen were employed to study impact air mass history on for wavelength λ=500 nm – AOT(500) and Ångström exponent. Backward trajectories computed, using NOAA HYSPLIT model, used trace history. It was found that spring, changes AOT values over strongly influenced by 8 days or longer duration, arriving both free troposphere an altitude 1 km above...

10.5194/acp-10-877-2010 article EN cc-by Atmospheric chemistry and physics 2010-02-01

In this work multi wavelength Raman lidar data from Ny-Ålesund, Spitsbergen have been analysed for the spring 2014 Arctic haze season, as part of iAREA campaign. Typical values and probability distributions aerosol backscatter, extinction depolarisation, ratio color 4 different altitude intervals within troposphere are given. These quantities their dependencies frequency altitude-dependent observed events A comparison with ground-based size distribution chemical composition is performed....

10.1016/j.atmosenv.2016.05.053 article EN cc-by Atmospheric Environment 2016-05-28

The results of studies the vertical gradient aerosol concentration measurements made during cruises r/v 'Oceania' between 2008 and 2012 are presented. Using from those experiments, sea spray emission fluxes were calculated for all particles sizes in range 0.5 μm to 8 μm, as well fifteen channels width. information obtained was further used calculate Sea Salt Generation Function (SSGF) Baltic depending on wind speed size distribution.

10.5697/oc.56-4.697 article EN cc-by-nc-nd Oceanologia 2014-01-01

The Poland-AOD aerosol research network was established in 2011 to improve aerosol–climate interaction knowledge and provide a real-time historical, comprehensive, quantitative database for the optical properties distribution over Poland. consists of institutions private owners operating 10 measurement stations an organization responsible model transport simulations. collaboration provides observations spectral depth (AOD), Ångstrom Exponent (AE), incoming shortwave (SW) longwave (LW)...

10.3390/atmos12121583 article EN cc-by Atmosphere 2021-11-27

Abstract. The aim of the presented study was to investigate impact on radiation budget a biomass-burning plume, transported from Alaska High Arctic region Ny-Ålesund, Svalbard, in early July 2015. Since mean aerosol optical depth increased by factor 10 above average summer background values, this large load event is considered particularly exceptional last 25 years. In situ data with hygroscopic growth equations, as well remote sensing measurements inputs radiative transfer models, were...

10.5194/acp-18-8829-2018 article EN cc-by Atmospheric chemistry and physics 2018-06-22

A five-year dataset of spectral aerosol optical thickness was used to analyse the seasonal variability properties (the (AOT) at wavelength λ = 500 nm, AOT(500) and Ångström exponent for 440–870 nm range, α(440, 870)) over Baltic Sea dependence these on meteorological factors (wind direction, wind speed relative humidity). The data from Gotland station global radiometric network AERONET (Aerosol Robotic Network, http://aeronet.gsfc.nasa.gov) were taken be representative conditions....

10.5697/oc.53-1.007 article EN cc-by-nc-nd Oceanologia 2011-03-01

Monte Carlo simulations of the expected influence nonuniformity in cloud structure and surface albedo on shortwave radiative fluxes Arctic atmosphere are presented. In particular, plane‐parallel biases transmittance studied for nonabsorbing, low‐level, all‐liquid stratus clouds over sea ice. The “absolute bias” is defined as difference between or uniform case, nonuniform conditions with same mean optical thickness albedo, averaged a given area (i.e., bias > 0 means overestimates). Ranges...

10.1029/2002jd002092 article EN Journal of Geophysical Research Atmospheres 2002-10-08

Abstract This paper addresses the influence of land topography and cover on 3D radiative effects under cloudless skies in Hornsund area, Spitsbergen, Svalbard. The authors used Monte Carlo simulations solar radiation transfer over a heterogeneous surface to study impact non-uniform on: (1) spatial distribution irradiance transmittance at fjord skies; (2) spectral shortwave aerosol forcing surface; (3) normalized nadir radiance Top Of Atmosphere (TOA) fjord. modelled transmittances radiances...

10.1515/popore-2017-0008 article EN cc-by-nc-nd Polish Polar Research 2017-06-27

This paper presents the results of Aerosol Optical Depth (AOD) studies which took place in Ny-Ålesund spring 2014 during iAREA campaign. The measurements were taken using Microtops II hand-held sunphotometers along Kongsfjorden, on a path leading from research village to fjord opening. Local breeze circulation was observed measurement campaign resulted an evident increase AOD profile towards open sea. Using AOD, changes over sea have been calculated and location front has determined.

10.1016/j.oceano.2017.04.005 article EN cc-by-nc-nd Oceanologia 2017-05-25

This paper estimates the influence of land topography and cover on 3D radiative effects under overcast skies in Arctic coastal environment, particular Hornsund fjord region, Spitsbergen. The authors focus impact a non-uniform surface on: (1) spatial distribution solar fluxes reaching surface, (2) spectral shortwave cloud forcing at (3) flux anomaly domain resulting from assumption uniform i.e. error due to plane parallel assumptions climate models, (4) remote sensing optical thickness over...

10.5697/oc.54-4.509 article EN cc-by-nc-nd Oceanologia 2012-11-01

Abstract. The aim of the presented study was to investigate impact on radiation budget biomass burning smoke plume transported from Alaska high Arctic region (Ny-Alesund, Svalbard) in early July 2015. This aerosol load event is considered exceptional last 25 years with mean optical depth increased by factor 10 comparison average summer background values. We utilised in-situ data hygroscopic growth equations as well remote sensing measurements inputs radiative transfer models an objective...

10.5194/acp-2017-1035 article EN cc-by 2017-11-17

Abstract. Black carbon (BC) is a significant forcing agent in the Arctic, but substantial uncertainty remains to quantify its climate effects due complexity of different mechanisms involved, particular related processes snowpack after deposition. In this study, we provide detailed and unique information on evolution variability BC content upper surface snow layer during spring period Svalbard (Ny-Ålesund). A total two snow-sampling strategies were adopted 2014 (from 1 April 24 June) specific...

10.5194/acp-21-12479-2021 article EN cc-by Atmospheric chemistry and physics 2021-08-19
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