Toward a minimal representation of aerosol direct and indirect effects (original) (raw)
Sign up for access to the world's latest research
checkGet notified about relevant papers
checkSave papers to use in your research
checkJoin the discussion with peers
checkTrack your impact
Sign up for access to the world's latest research
Related papers
Aerosol thermooptical characteristics in different types of aerosol weather
26th International Symposium on Atmospheric and Ocean Optics, Atmospheric Physics, 2020
The grand partition functions of ABJ theory can be factorized into even and odd parts under the reflection of fermion coordinate in the Fermi gas approach. In some cases, the even/odd part of ABJ grand partition function is equal to that of N = 5 O(n) × USp(n ) theory, hence it is natural to think of the even/odd projection of grand partition function as an orientifolding of ABJ Fermi gas system. By a systematic WKB analysis, we determine the coefficients in the perturbative part of grand potential of such orientifold ABJ theory. We also find the exact form of the first few "half-instanton" corrections coming from the twisted sector of the reflection of fermion coordinate. For the Chern-Simons level k = 2, 4, 8 we find closed form expressions of the grand partition functions of orientifold ABJ theory, and for k = 2, 4 we prove the functional relations among the grand partition functions conjectured in arXiv:1410.7658.
Atmospheric Chemistry and Physics, 2011
In this paper we describe and summarize the main achievements of the European Aerosol Cloud Climate and Air Quality Interactions project (EUCAARI). EUCAARI started on 1 January 2007 and ended on 31 December 2010 leaving a rich legacy including: (a) a comprehensive database with a year of observations of the physical, chemical and optical properties of aerosol particles over Europe, (b) comprehensive aerosol measurements in four developing countries, (c) a database of airborne measurements of aerosols and clouds over Europe during May 2008, (d) comprehensive modeling tools to study aerosol processes fron nano to global scale and their effects on climate and air quality. In addition a new Pan-European aerosol emissions inventory was developed and evaluated, a new cluster spectrometer was built and tested in the field and several new aerosol parameterizations and computations modules for chemical transport and global climate models were developed and evaluated. These achievements and related studies have substantially improved our understanding and reduced the uncertainties of aerosol radiative forcing and air quality-climate interactions. The EUCAARI results can be utilized in European and global environmental policy to assess the aerosol impacts and the corresponding abatement strategies.
Comparison of Intercontinental Aerosols: Desert and Monsoon-Influenced Regions
Physical Science International Journal, 2017
AIM: This research project was undertaken to compare the optical and physical properties of aerosols at the 0.440 μm, 0.675 μm, 0.870 μm and 1.020 μm spectral wavelengths between desert and monsoon-influenced regions. In this project, Zinder, one of the popular cities in the Republic of Niger and Beijing, the capital city of China were chosen to represent desert and monsooninfluenced regions respectively. Place and Duration of Study: Four years of Aerosol Optical Depth (AOD) data were extracted from level 2.0, the quality-assured almucantar version products of AERONET data, at both Beijing-CAMS (39.933°N, 116.317°E) and Zinder Airport (13.775°N, 8.984°E) between 2012 and 2015. Methodology: In this research project, physical and optical properties of aerosols were determined using Angstrom equations. Angstrom exponent, curvature, turbidity coefficient and spectral variation of the aerosols in Zinder Airport and Beijing-CAMS were calculated and the results were then compared. Both the physical and optical properties of the aerosols were determined from the calculated values. Results: The results obtained indicated that there were dominant coarse-mode aerosol particles in Zinder city, while fine-mode aerosol particles were found in Beijing. The results also showed that the overall Aerosol Optical Depth (AOD) in Zinder is higher than that of Beijing, but the atmosphere of Beijing was hazier than that of Zinder. The prevalence of coarse-mode particle sizes in Zinder was due to desert dust particles in the region, while the prevalence of fine-mode particles in Beijing was due to anthropogenic aerosol particle generation in the region, which may result from heavy industrialization in China. The higher aerosol loading in Zinder is responsible for absorbing light coming from the sun which, in turn, makes the atmosphere clear, while the lower aerosol loading in Beijing is responsible for scattering light coming from the sun, thereby obstructing the atmospheric visibility in the region.
Loading Preview
Sorry, preview is currently unavailable. You can download the paper by clicking the button above.