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1

Institute for the Study of Earth, Ocean, and Space, University of New Hampshire, Durham, NH 03824, USA

2

Department of Physical Oceanography, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA

3

Department of Earth and Atmospheric Sciences, University of Houston, Houston, TX 77204, USA

4

Department of Chemistry, SUNY-College of Environmental Sciences and Forestry, Syracuse, NY 13210, USA

5

Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, and NOAA Earth System Research Laboratory, Boulder, CO 80305, USA





*

Author to whom correspondence should be addressed.



Abstract An analysis of coastal meteorological mechanisms facilitating the transit pollution plumes emitted from sources in the Northeastern U.S. was based on observations from the International Consortium for Atmospheric Research on Transport and Transformation ICARTT 2004 field campaign. Particular attention was given to the relation of these plumes to coastal transport patterns in lower tropospheric layers throughout the Gulf of Maine GOM, and their contribution to large-scale pollution outflow from the North American continent. Using measurements obtained during a series of flights of the National Oceanic and Atmospheric Administration NOAA WP-3D and the National Aeronautics and Space Administration NASA DC-8, a unique quasi-Lagrangian case study was conducted for a freshly emitted plume emanating from the New York City source region in late July 2004. The development of this plume stemmed from the accumulation of boundary layer pollutants within a coastal residual layer, where weak synoptic conditions allowed for its advection into the marine troposphere and transport by a mean southwesterly flow. Upon entering the GOM, analysis showed that the plume layer vertical structure evolved into an internal boundary layer form, with signatures of steep vertical gradients in temperature, moisture and wind speed often resulting in periodic turbulence. This structure remained well-defined during the plume study, allowing for the detachment of the plume layer from the surface and minimal plume-sea surface exchange. In contrast, shear driven turbulence within the plume layer facilitated lateral mixing with other low-level plumes during its transit. This turbulence was periodic and further contributed to the high spatial variability in trace gas mixing ratios. Further influences of the turbulent mixing were observed in the impact of the plume inland as observed by the Atmospheric Investigation, Regional Modeling, Analysis and Prediction AIRMAP air quality network. This impact was seen as extreme elevations of surface ozone and CO levels, equaling the highest observed that summer. View Full-Text

Keywords: coastal; atmospheric physics; continental outflow; trace gas transport; turbulence; boundary layers; ICARTT campaign; New England; North Atlantic; Lagrangian; regional climate coastal; atmospheric physics; continental outflow; trace gas transport; turbulence; boundary layers; ICARTT campaign; New England; North Atlantic; Lagrangian; regional climate





Autor: Shannon R. Davis 1,2,* , Robert Talbot 3, Huiting Mao 4 and Jonathan A. Neuman 5

Fuente: http://mdpi.com/



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