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Trans-Pacific transport of Asian dust and CO: accumulation of biomass burning CO in the subtropics and dipole structure of transport
Trans-Pacific transport Asian dust and CO biomass burning CO the subtropics and dipole structure of transport
2010/8/12
In May 2003, both MODIS aerosol optical depth (AOD) and carbon monoxide (CO) measurements from MOPITT show significant trans-Pacific transport to North America. We apply the global chemical transport ...
Large scale features associated with strong frontogenesis in equivalent potential temperature in the South American subtropics east of the Andes
strong frontogenesis equivalent potential temperature South American subtropics east Andes
2010/1/28
South American subtropics east of the Andes exhibit a region of intense climatological frontogenesis in equivalent potential temperature (EPT) in the December to March season, mostly produced by defor...
A quantitative evaluation of the role of the Argentinean Col and the Low Pressure Tongue East of the Andes for frontogenesis in the South American subtropics
Argentinean Col Low Pressure Tongue East South American subtropics
2010/1/28
Previous studies have found the South American subtropics to exhibit high climatological frontogenesis in equivalent potential temperature during the austral summer. An important contribution to this ...
An unusual stratospheric ozone decrease in the Southern Hemisphere subtropics linked to isentropic air-mass transport as observed over Irene (25.5° S, 28.1° E) in mid-May 2002
unusual stratospheric ozone decrease Southern Hemisphere subtropics sentropic air-mass transport
2009/1/8
A prominent ozone minimum of less than 240 Dobson Units (DU) was observed over Irene (25.5° S, 28.1° E), a subtropical site in the Southern Hemisphere, by the Total Ozone Mapping Spectrometer (TOMS) d...
Downscaling heavy rainfall in the subtropics – a simple approach for dynamical nesting
heavy rainfall subtropics simple approach dynamical nesting
2010/1/26
The simulation of local scale precipitation with nested models often suffers from large errors in the boundary rows. Advection of precipitation into the model domain of the small scale model can lead ...