نتایج جستجو برای: atmospheric aerosol

تعداد نتایج: 100598  

2015
Bonnie K. Ellis James A. Craft Jack A. Stanford

We documented significantly increasing trends in atmospheric loading of ammonium (NH4) and nitrate/nitrite (NO2/3) and decreasing trends in total phosphorus (P) and sulfate (SO4) to Flathead Lake, Montana, from 1985 to 2004. Atmospheric loading of NO2/3 and NH4 increased by 48 and 198% and total P and SO4 decreased by 135 and 39%. The molar ratio of TN:TP also increased significantly. Severe ai...

2015
W. T. Morgan B. Ouyang J. D. Allan E. Aruffo P. Di Carlo O. J. Kennedy D. Lowe M. J. Flynn P. D. Rosenberg P. I. Williams R. Jones G. B. McFiggans

Aerosol chemical composition was found to influence nighttime atmospheric chemistry during a series of airborne measurements in northwestern Europe in summer conditions, which has implications for regional air quality and climate. The uptake of dinitrogen pentoxide, γ (N2O5), to particle surfaces was found to be modulated by the amount of water content and ammonium nitrate present in the aeroso...

2017
Nataliia Borodai

Satellite instruments are commonly used for measurements of aerosol optical properties in the atmosphere. In this work we use such measurements for ultra-high energy cosmic ray studies. We introduce a method of preparation of aerosol maps for the location of the Pierre Auger Observatory. For these maps the data from the Ozone Monitoring Instrument (OMI) of the Aura satellite were analyzed for t...

Journal: :Proceedings of the National Academy of Sciences of the United States of America 2013
Gabriela Adler Thomas Koop Carynelisa Haspel Ilya Taraniuk Tamar Moise Ilan Koren Reuven H Heiblum Yinon Rudich

The cycling of atmospheric aerosols through clouds can change their chemical and physical properties and thus modify how aerosols affect cloud microphysics and, subsequently, precipitation and climate. Current knowledge about aerosol processing by clouds is rather limited to chemical reactions within water droplets in warm low-altitude clouds. However, in cold high-altitude cirrus clouds and an...

2010
Abhijit Chatterjee Anandamay Adak Ajay K. Singh Manoj K. Srivastava Sanjay K. Ghosh Suresh Tiwari Panuganti C. S. Devara Sibaji Raha

BACKGROUND There is an urgent need for an improved understanding of the sources, distributions and properties of atmospheric aerosol in order to control the atmospheric pollution over northeastern Himalayas where rising anthropogenic interferences from rapid urbanization and development is becoming an increasing concern. METHODOLOGY/PRINCIPAL FINDINGS An extensive aerosol sampling program was...

2010
Zhaobing Guo Zhanqing Li James Farquhar Alan J. Kaufman Nanping Wu Can Li Russell R. Dickerson Pucai Wang

[1] Atmospheric sulfate aerosols have a cooling effect on the Earth’s surface and can change cloud microphysics and precipitation. China has heavy loading of sulfate, but their sources and formation processes remain uncertain. In this study we characterize possible sources and formation processes of atmospheric sulfate by analyzing sulfur isotope abundances (S, S, 34S, and S) and by detailed X‐...

Journal: :Proceedings of the National Academy of Sciences of the United States of America 2012
Pablo E Saide Gregory R Carmichael Scott N Spak Patrick Minnis J Kirk Ayers

Limitations in current capabilities to constrain aerosols adversely impact atmospheric simulations. Typically, aerosol burdens within models are constrained employing satellite aerosol optical properties, which are not available under cloudy conditions. Here we set the first steps to overcome the long-standing limitation that aerosols cannot be constrained using satellite remote sensing under c...

2013
L. D. Yee K. E. Kautzman C. L. Loza K. A. Schilling M. M. Coggon P. S. Chhabra M. N. Chan A. W. H. Chan S. P. Hersey

The formation of secondary organic aerosol from oxidation of phenol, guaiacol (2-methoxyphenol), and syringol (2,6-dimethoxyphenol), major components of biomass burning, is described. Photooxidation experiments were conducted in the Caltech laboratory chambers under low-NOx (< 10 ppb) conditions using H2O2 as the OH source. Secondary organic aerosol (SOA) yields (ratio of mass of SOA formed to ...

2005
V. S. Kozlov

BC is the predominant source of solar absorption in atmospheric aerosol, which impacts climate. (Jacobson 2001; Rozenberg 1982). In this paper, we analyze the results of laboratory and field investigations that focused on the relative content of BC in aerosol particles. Main attention is given to the study of possibility using this parameter as an informative sign for estimating the effect of r...

نمودار تعداد نتایج جستجو در هر سال

با کلیک روی نمودار نتایج را به سال انتشار فیلتر کنید