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The Effect of Aerosols on the Climate

The Effect of Aerosols on the Climate. By Hugh Alvarado Student Researchers: Juan Rodrigez, Irving Andino, Johan Toloza Faculty Mentors: Dr. James Frost 1 , Dr. Elizabeth Rudolph 2 , and Mr. Ryan Hutchinson 3

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The Effect of Aerosols on the Climate

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  1. The Effect of Aerosols on the Climate By Hugh Alvarado Student Researchers: Juan Rodrigez, Irving Andino, Johan Toloza Faculty Mentors: Dr. James Frost1, Dr. Elizabeth Rudolph2, and Mr. Ryan Hutchinson3 1LaGuardia Community College: 31-10 Thomson Avenue, Long Island City, New York 11101   2City College: New York, New York   3Medgar Evers College: 1150 Carroll Street, Brooklyn, NY 11225   of the City University of New York

  2. Abstract • Aerosols in our atmosphere can affect our climate both directly and indirectly. • The direct effect can cause climate forcing by absorbing and reflecting sunlight, therefore, cooling the atmosphere. While the indirect effect modifies cloud properties. • With the help of the handheld Polarimeter in conjunction  with the automated CIMEL sun photometer, we can effectively determine the optical depth and size of aerosol particles. 

  3. Introduction What are Aerosols? • Aerosols are tiny solid or liquid particles suspended in the air. These are often seen by the naked eye as smoke, haze and dust. Some occur naturally, originating from volcanoes, dust storms, forest and grassland fires, living vegetation, and sea spray. • However, a greater percentage of aerosol particles originate from Human activities, such as the burning of fossil fuels and the alteration of the natural surface cover.

  4. Aerosols Properties • However, the problem with aerosols is that they have a great variety of properties, which makes them difficult to identify, locate, and classify. • Aerosols divide into, Troposheric and Stratospheric aerosols. • Aerosols differ in size, chemical composition, and lifetime.

  5. Troposperic Aerosols Aerosols located in the troposphere, these are mainly anthropogenic. This type of aerosol varies in size and chemical composition, according to the region where it is located. Have a direct effect on the climate. Stratospheric Aerosol Aerosols located in the higher zone of the lower atmosphere. This type of aerosols affect the properties of clouds. Have an indirect effect on the climate. Types of Aerosols

  6. Climatic Effect of Aerosols(Problem)

  7. Tropospheric and Stratospheric Aerosols

  8. Methodology • In this project we used a Hand-Held Polarimeter to measure the refractive index, optical depth, and particle size (radius) of aerosols. To test the accuracy of our data, we compared the data obtained from the Polarimeter, with data obtained from a CIMEL sun photometer. • The data is collected by aiming the Polarimeter toward the sun at different angles. At the same time, we rotated the Polarimeter to determine the Imax and Imin values. Finally, we analyzed the data obtained using IDL (computer program) to determine the optical depth and size of the particles.

  9. Polarimeter

  10. 05_07_11  cloudy Angle    Imax   Imin 30        161     153 40        115     105 50        92       73 60        79       73 70        72       42 80        72       36 90        89       61 05_07_12 clear Angle    Imax   Imin 30        165     152 40        144     118 50        125      90 60        111      73 70        105      60 80        106      55 90        119      61 Results • Data: • Comparison of data taken at the same place on different days (and under varying weather conditions). These charts represent the values for the data acquired on July 11, 2005 and July 12, 2005. • Blue color filter used

  11. Data After analyzing the data obtained from both days, we discovered that the aerosol particles from July 12, 2005, have greater radii and optical depth than the particles from July 11, 2005.

  12. Discussion • Although ideally we would be able to clear the atmosphere of harmful aerosols, such an option is unavailable. • However, there are solutions to depress the presence of aerosols in the atmosphere. Laws can be enacted by the major industrial countries around the world to limit aerosol ejection by reducing the use of fuels, energy, and the production of waste. Implementing laws that regulate the use of raw materials and require the use of renewable resources will give scientist more time to analyze aerosols and develop methods to clear them from our atmosphere before aerosols reach dangerously high levels.

  13. Conclusion • After analyzing the data collected with the Polarimeter, we can concur that aerosols can change in size and optical depth in a matter of hours if not seconds. Similarly, we hypothesized that aerosols modify the properties of clouds. By comparing the amount of energy measured on July 11th with the measurements taken on July 12th , we concluded that less energy reaches the earth on cloudy days, than it does on clear days.

  14. Future Work • To collect data using instruments that analyze chemical composition, refractive index, and optical depth of aerosols. • Investigate the purpose of sulfur in the aerosols. • Continue gathering data to develop weather models.

  15. Acknowledgements • Dr. Rudolph, Dr. Frost • Juan Rodrigez, Irving Andino, Johan Toloza • NASA Sharp

  16. Bibliography • Dr. James Frost. Aerosol Project at La Guardia.Online. La Guardia Community College. http://www.cis.lagcc.cuny.edu/frost/html/ • Center for Atmospheric Sciences. Online. NASA and NOAA. http://cas.hamptonu.edu/research/topics/5-6aersols.html

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