|
Read Full Article (file size: 698673 bytes) Cited by
JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 111,
D03105,
doi:10.1029/2005JD006006,
2006
Role of convection in global-scale transport in the troposphere
Tatiana Erukhimova
Department of Atmospheric Sciences, Texas A&M University, College Station, Texas, USA
Kenneth P. Bowman
Department of Atmospheric Sciences, Texas A&M University, College Station, Texas, USA
Abstract
The role of convection in global-scale transport in the troposphere is studied by using climatological Green's functions of
the mass conservation equation for a conserved, passive tracer. The Green's functions are calculated from long-term atmospheric
trajectory calculations based on three-dimensional winds from a 19-year simulation by Version 3 of the NCAR Community Climate
Model (CCM3). Two trajectory calculations are compared: one that includes the effects of the model's parameterized convection
and one that neglects the convective transport. The global transport properties of the two cases are qualitatively similar.
The global troposphere can be divided into three parts: the tropics, and the Northern and Southern Hemisphere extratropics.
Transport within each region is rapid, while the exchange of air between the regions is comparatively slow. Semipermeable
barriers to transport exist in the subtropics in both cases. Convection slightly suppresses transport across the subtropical
barriers. Convective transport enhances the vertical dispersion of air parcels, particularly in the rising branch of the Hadley
circulation. Localized differences between the two runs can reach 50–80%. The differences are largest in the upper troposphere.
Interannual transport variations related to the El Niño–Southern Oscillation (ENSO) phase can be detected in both cases, with
the vertical transport being enhanced in the presence of convection.
Received 22
March
2005;
accepted 14
November
2005;
published 11
February
2006.
Keywords: transport;
troposphere;
convection.
Index Terms: 0368 Atmospheric Composition and Structure: Troposphere: constituent transport and chemistry; 3314 Atmospheric Processes: Convective processes; 3337 Atmospheric Processes: Global climate models (1626, 4928); 3309 Atmospheric Processes: Climatology (1616, 1620, 3305, 4215, 8408).
Read Full Article (file size: 698673 bytes) Cited by
Citation: Erukhimova, T., and K. P. Bowman
(2006),
Role of convection in global-scale transport in the troposphere,
J. Geophys. Res.,
111,
D03105,
doi:10.1029/2005JD006006.
Copyright 2006 by the American Geophysical Union.
|