HR: 1340h
AN: A13C-1362    [Abstracts]
TI: Factors Influencing Aerosol Concentrations and Properties over the Tropical Eastern Pacific: Observations from TC4
AU: Anderson, B E
EM: bruce.e.anderson@nasa.gov
AF: NASA Langley Research Center, MS 483 NASA LaRC, Hampton, VA 23681, United States
AU: * Chen, G
EM: gao.chen@nasa.gov
AF: NASA Langley Research Center, MS 483 NASA LaRC, Hampton, VA 23681, United States
AU: Thornhill, K L
EM: kenneth.l.thornhill@nasa.gov
AF: SSAI, MS 483 NASA Langley Research Center, Hampton, VA 23681, United States
AU: Winstead, E L
EM: edward.l.winstead@nasa.gov
AF: SSAI, MS 483 NASA Langley Research Center, Hampton, VA 23681, United States
AU: Dibb, J
EM: jack.dibb@unh.edu
AF: University of New Hampshire, Morse Hall 39 College Road, Durham, NH 03824-3525, United States
AU: Scheuer, E
EM: eric.scheuer@unh.edu
AF: University of New Hampshire, Morse Hall 39 College Road, Durham, NH 03824-3525, United States
AU: Lathem, T
EM: terry.lathem@gmail.com
AF: Georgia Institute of Technology, School of Earth and Atmospheric Sciences 311 Ferst Drive, Atlanta, GA 30332, United States
AB: The NASA Tropical Composition Cloud and Climate Coupling (TC4) mission was conducted during summer 2007 and had the primary objective of gaining a better understanding of composition and dynamics of the upper troposphere over the tropical eastern pacific region. Based in San Jose, Costa Rica, the mission employed instrumented aircraft along with ground, balloon, and satellite borne sensors to determine the spatial distribution of trace gas and aerosol species as well as moisture and clouds between the surface and roughly 16 km altitude over Central America, the eastern Pacific, the western Caribbean and northern South America. Because of its heavy payload and long endurance capability, the NASA DC-8 aircraft was the primary sampling platform for the lower-tropospheric altitude regime (i.e., below 12 km). It carried both remote and in situ instruments and was used to characterize cloud inflow and outflow as well as the microphysical properties of maritime convective systems. Because of their roles in regulating atmospheric radiation transfer and cloud formation and microphysics, flight plans placed particular emphasis on determining the sources and properties of the aerosol particles present within the region. A preliminary analysis of the DC-8 data set suggests that the following sources/processes had the greatest impact on aerosol number and mass loading: dust transport from Africa; sea salt production over the ocean; urban and biogenic emissions over the continent; secondary aerosol formation in volcanic plumes; nucleation in cloud outflow; and cloud scavenging. In this presentation, we will examine the microphysical, optical and hydration properties of each aerosol type and assess the overall impact of the source/sink processes to the regional aerosol budget. We will also contrast the microphysical properties of the Saharan Dust sampled over the Caribbean with those measured in fresh dust layers over the eastern Atlantic from the DC-8 during the summer 2006, NASA African Monsoon Multidisciplinary Activity (NAMMA).
DE: 0300 ATMOSPHERIC COMPOSITION AND STRUCTURE
DE: 0305 Aerosols and particles (0345, 4801, 4906)
SC: Atmospheric Sciences [A]
MN: 2007 Fall Meeting