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HSRL ARCTAS Spring 2008 FIELD CAMPAIGN

NAAMES
SABOR
DISCOVER-AQ
MILAGRO
GoMACCS/TexAQS
CALIPSO-Val
San Joaquin Valley
CHAPS
CALIPSO/CATZ/MODIS
Caribbean-CALIPSO
ARCTAS Spring
ARCTAS Summer
 
The Arctic Research of the Composition of the Troposphere from Aircraft and Satellites (ARCTAS) mission is aimed at learning more about the state of the Arctic atmosphere and reporting on the changes that have occurred as a result of pollution. Because the accumulation of northern mid-latitude pollution is at a peak in April, ARCTAS will focus its spring deployment on the environmental consequences.
Radiative forcing from thick aerosol layers ("arctic haze") and black carbon deposition to snow modify regional and global climate. Seasonal build-up of tropospheric ozone and its precursors affects the ozone budget on a hemispheric scale. In addition, the deposition of mercury transported from mid-latitudes is a recognized threat to arctic ecosystems.
While we know these problems exist, there remain large uncertainties regarding the transport pathways from mid-latitudes to the Arctic, and the relative contributions of different source regions to arctic pollution. Integration of satellite and aircraft observations with models through ARCTAS provides a means to address this issue.
For more information about ARCTAS from Researcher News, visit:   https://www.nasa.gov/centers/langley/news/researchernews/rn_ARCTAS.html.

For the ARCTAS Project home page hosted by the Earth Science Project Office(ESPO) at NASA Ames, visit: http://www.espo.nasa.gov/arctas/


MARCH 2008 PRELIMINARY & TRANSIT FLIGHTS
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Flight
13
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17
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30
Flight L1
Flight L2
Flight L3
31
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Flight L2


APRIL 2008 SCHEDULE
Sun Mon Tue Wed Thu Fri Sat
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Flight L1
Flight L2
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Flight L2
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Funding for the deployment of the NASA King Air was provided by NASA and the Department of Energy (DOE) Atmospheric Science Program. Logistical support was provided by NOAA ESRL. The information contained herein is provided as a public service, with the understanding that NASA, DOE, NOAA, and the ARCTAS project collaborators make no warranties, either expressed or implied, concerning the accuracy, completeness, reliability, or suitability of the information. Do not quote or cite without permission. Permission for use of these data and additional information may be obtained from the investigating scientists: Chris Hostetler, Richard Ferrare, or John Hair. The data are preliminary and subject to change.