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AGU: Journal of Geophysical Research, Atmospheres

 

Keywords

  • aerosol optical depth Sun photometer measurements
  • polar aerosol characterization
  • radiative and chemical composition parameters of polar aerosols

Index Terms

  • Atmospheric Composition and Structure: Aerosols and particles
  • Global Change: Atmosphere
  • Atmospheric Composition and Structure: Troposphere: composition and chemistry
  • Atmospheric Processes: Radiative processes
Abstract
Cited By (24)
 

Abstract

JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 112, D16205, 28 PP., 2007
doi:10.1029/2007JD008432

Aerosols in polar regions: A historical overview based on optical depth and in situ observations

C. Tomasi

Institute of Atmospheric Sciences and Climate, Consiglio Nazionale delle Ricerche, Bologna, Italy

V. Vitale

Institute of Atmospheric Sciences and Climate, Consiglio Nazionale delle Ricerche, Bologna, Italy

A. Lupi

Institute of Atmospheric Sciences and Climate, Consiglio Nazionale delle Ricerche, Bologna, Italy

C. Di Carmine

Institute of Atmospheric Sciences and Climate, Consiglio Nazionale delle Ricerche, Bologna, Italy

M. Campanelli

Institute of Atmospheric Sciences and Climate, Consiglio Nazionale delle Ricerche, Rome, Italy

A. Herber

Alfred Wegener Institute of Polar and Marine Research, Bremerhaven, Germany

R. Treffeisen

Alfred Wegener Institute of Polar and Marine Research, Potsdam, Germany

R. S. Stone

Global Monitoring Division, NOAA, Boulder, Colorado, USA

E. Andrews

Global Monitoring Division, NOAA, Boulder, Colorado, USA

S. Sharma

Science and Technology Branch, Environment Canada, Toronto, Ontario, Canada

V. Radionov

Arctic and Antarctic Research Institute, St. Petersburg, Russia

W. von Hoyningen-Huene

Institute of Environmental Physics/Remote Sensing, University of Bremen, Bremen, Germany

K. Stebel

Polar Environmental Centre, Norwegian Institute for Air Research, Tromsø, Norway

G. H. Hansen

Polar Environmental Centre, Norwegian Institute for Air Research, Tromsø, Norway

C. L. Myhre

Polar Environmental Centre, Norwegian Institute for Air Research, Tromsø, Norway

C. Wehrli

Physikalisch-Meteorologisches Observatorium/World Radiation Centre, Davos, Switzerland

V. Aaltonen

Finnish Meteorological Institute, Helsinki, Finland

H. Lihavainen

Finnish Meteorological Institute, Helsinki, Finland

A. Virkkula

Finnish Meteorological Institute, Helsinki, Finland

R. Hillamo

Finnish Meteorological Institute, Helsinki, Finland

J. Ström

Department of Applied Environmental Science, Stockholm University, Stockholm, Sweden

C. Toledano

Grupo de Óptica Atmosférica, Universidad de Valladolid, Valladolid, Spain

V. E. Cachorro

Grupo de Óptica Atmosférica, Universidad de Valladolid, Valladolid, Spain

P. Ortiz

Grupo de Óptica Atmosférica, Universidad de Valladolid, Valladolid, Spain

A. M. de Frutos

Grupo de Óptica Atmosférica, Universidad de Valladolid, Valladolid, Spain

S. Blindheim

Andoya Rocket Range, Andenes, Norway

M. Frioud

Andoya Rocket Range, Andenes, Norway

M. Gausa

Andoya Rocket Range, Andenes, Norway

T. Zielinski

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

T. Petelski

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

T. Yamanouchi

National Institute of Polar Research, Tokyo, Japan

Large sets of filtered actinometer, filtered pyrheliometer and Sun photometer measurements have been carried out over the past 30 years by various groups at different Arctic and Antarctic sites and for different time periods. They were examined to estimate ensemble average, long-term trends of the summer background aerosol optical depth AOD(500 nm) in the polar regions (omitting the data influenced by Arctic haze and volcanic eruptions). The trend for the Arctic was estimated to be between −1.6% and −2.0% per year over 30 years, depending on location. No significant trend was observed for Antarctica. The time patterns of AOD(500 nm) and Ångström's parameters α and β measured with Sun photometers during the last 20 years at various Arctic and Antarctic sites are also presented. They give a measure of the large variations of these parameters due to El Chichon, Pinatubo, and Cerro Hudson volcanic particles, Arctic haze episodes most frequent in winter and spring, and the transport of Asian dust and boreal smokes to the Arctic region. Evidence is also shown of marked differences between the aerosol optical parameters measured at coastal and high-altitude sites in Antarctica. In situ optical and chemical composition parameters of aerosol particles measured at Arctic and Antarctic sites are also examined to achieve more complete information on the multimodal size distribution shape parameters and their radiative properties. A characterization of aerosol radiative parameters is also defined by plotting the daily mean values of α as a function of AOD(500 nm), separately for the two polar regions, allowing the identification of different clusters related to fifteen aerosol classes, for which the spectral values of complex refractive index and single scattering albedo were evaluated.

Received 18 January 2007; accepted 30 May 2007; published 21 August 2007.

Citation: Tomasi, C., et al. (2007), Aerosols in polar regions: A historical overview based on optical depth and in situ observations, J. Geophys. Res., 112, D16205, doi:10.1029/2007JD008432.

Cited By

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