Advances in Meteorology

Atmospheric Aerosols and Climate


Publishing date
01 Nov 2010
Status
Published
Submission deadline
01 May 2010

1Atmospheric Research Team, Institute of Environmental Research and Sustainable Development, National Observatory of Athens, Lofos Nymphon, P.O. Box 20048, 11810 Athens, Greece

2Group of Atmospheric Optics, Department of Optics and Applied Physics, Faculty of Sciences, University of Valladolid, Prado de la Magdalena S/N, 47071 Valladolid, Spain

3Max Planck Institute for Meteorology, Bundesstraße 55, 20146 Hamburg, Germany

4Space Physics Laboratory, Vikram Sarabhai Space Center, Department of Space, 695022 Trivandrum, India

5Climate Change Unit, Finnish Meteorological Institute, P.O. Box 503, 00101 Helsinki, Finland

6Institute of Atmospheric Sciences and Climate, National Council of Research, Via Gobetti 101, 41029 Bologna, Italy


Atmospheric Aerosols and Climate

Description

Atmospheric aerosols affect the Earth's radiation budget directly by scattering and absorbing the solar and terrestrial radiation, and indirectly by modifying the physical and radiative properties of clouds. Through their combined direct and indirect effects, anthropogenic aerosols have the potential to cause climate forcing comparable in magnitude, but opposite in sign, to that caused by anthropogenic emissions of greenhouse gases.

The anthropogenic aerosol optical depth has increased by about 50% on an annual basis at global scale since the preindustrial era. At regional scale, however, this increase varies significantly, with the largest increases being observed in urban areas.

Aerosols in areas influenced by anthropogenic activities are physically and chemically different from those in remote areas. These differences influence the aerosol optical properties, including scattering, absorption, single scattering albedo, and phase function, all as functions of wavelength. Knowledge on the aerosol properties is important for modeling the aerosol radiative effects on climate and retrieving the aerosol optical properties using remote-sensing techniques. Besides, changes in the vertical structure of the atmosphere lead to formation of distinct layers of aerosols above the planetary boundary layer; these aerosols are transported to long distances under favorable conditions. The radiative implications of such elevated aerosols have immense impact on regional weather and climate.

The role of atmospheric aerosols in the Earth's climate system remains uncertain. Therefore, the special issue on Atmospheric Aerosols and Climate intends to provide the scientific community with a forum to present up-to-date research results, including studies on the behavior of atmospheric aerosols in the Earth's climate system. The topics to be covered include, but are not limited to:

  • Experimental and modeling techniques for the study of aerosol optical characteristics, from microphysical to radiative properties
  • Influence of the aerosol characteristics on climate and weather modification
  • Experimental techniques including ground-based and airborne in-situ and remote-sensing measurements as well as satellite retrievals

Before submission authors should carefully read over the journal's Author Guidelines, which are located at http://www.hindawi.com/journals/amet/guidelines/. Prospective authors should submit an electronic copy of their complete manuscript through the journal Manuscript Tracking System at http://mts.hindawi.com/ according to the following timetable:


Articles

  • Special Issue
  • - Volume 2010
  • - Article ID 708782
  • - Editorial

Atmospheric Aerosols and Climate

Harry D. Kambezidis | Victoria E. Cachorro | ... | Vito Vitale
  • Special Issue
  • - Volume 2010
  • - Article ID 681587
  • - Research Article

Urban Surface Temperature Reduction via the Urban Aerosol Direct Effect: A Remote Sensing and WRF Model Sensitivity Study

Menglin Jin | J. Marshall Shepherd | Weizhong Zheng
  • Special Issue
  • - Volume 2010
  • - Article ID 154368
  • - Research Article

An Assessment of the Efficiency of Dust Regional Modelling to Predict Saharan Dust Transport Episodes

D. K. Papanastasiou | A. Poupkou | ... | J. M. Baldasano
  • Special Issue
  • - Volume 2010
  • - Article ID 139186
  • - Research Article

Assessment of Aerosol Radiative Impact over Oceanic Regions Adjacent to Indian Subcontinent Using Multisatellite Analysis

S. K. Satheesh | V. Vinoj | K. Krishnamoorthy
  • Special Issue
  • - Volume 2010
  • - Article ID 760546
  • - Research Article

Diagnosis of the Relationship between Dust Storms over the Sahara Desert and Dust Deposit or Coloured Rain in the South Balkans

N. G. Prezerakos | A. G. Paliatsos | K. V. Koukouletsos
  • Special Issue
  • - Volume 2010
  • - Article ID 812075
  • - Research Article

Vertical and Horizontal Gradients in Aerosol Black Carbon and Its Mass Fraction to Composite Aerosols over the East Coast of Peninsular India from Aircraft Measurements

S. Suresh Babu | K. Krishna Moorthy | S. K. Satheesh
  • Special Issue
  • - Volume 2010
  • - Article ID 147910
  • - Research Article

Aerosol Monitoring over Athens Using Satellite and Ground-Based Measurements

D. G. Kaskaoutis | N. Sifakis | ... | H. D. Kambezidis
  • Special Issue
  • - Volume 2010
  • - Article ID 168346
  • - Research Article

Identification of the Aerosol Types over Athens, Greece: The Influence of Air-Mass Transport

D. G. Kaskaoutis | P. G. Kosmopoulos | ... | P. T. Nastos
Advances in Meteorology
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Acceptance rate14%
Submission to final decision121 days
Acceptance to publication18 days
CiteScore4.600
Journal Citation Indicator0.490
Impact Factor2.9
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