Vertical distribution of aerosols in the vicinity of Mexico City during MILAGRO-2006 Campaign

Significant diurnal variations of aerosol light absorption and scattering were ob- served and are attributed in part due to changes in the meteorology in the Mexico City Basin and

M.: Measurements of black carbon specific absorption in the Mexico City Metropolitan Area during the MCMA 2003 field campaign, Atmos. J.: Estimation of a “radiatively correct”

(2009) coupled fast measurements of aerosol and gas-phase constituents with the ISORROPIA-II thermodynamic model to study the partitioning of semivolatile inorganic species and

As part of the Megacity Initiative: Local and Global Re- search Observations (MILAGRO) 2006 field campaign, we measured the fluxes (positive emission fluxes and nega- tive

The aircraft measurements from the NSF/NCAR C-130 and the NASA DC-8 sampled both the Mexico City urban area and the surrounding region over Mexico and the Gulf of Mexico,

Although the WRF-CHEM model follows well the variation of OH concentrations, it underestimates the OH concentrations in the late morning and early afternoon, regardless of whether

L.: Mexico City aerosol analysis during MILAGRO using high resolution aerosol mass spectrometry at the urban supersite (T0) – Part 1: Fine particle composition and organic

Fast measurements of aerosol and gas-phase constituents coupled with the ISORROPIA-II thermodynamic equilibrium model are used to study the partitioning of semivolatile