Chemically-resolved aerosol eddy covariance flux measurements in urban Mexico City during MILAGRO 2006

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

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

(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

that had been ionized by charge transfer or had humidity dependent ion mass peak signals. Humidity dependent class-B fluxes were observed for several ions including protonated di-

Fluxes measured by both methods during the night in the fall are small, with a upward flux measured using the EC method and downward fluxes measured by the MBR method in all

Long-term measurements of carbon dioxide flux ( F c ) and the latent and sensible heat fluxes were performed using the eddy covariance (EC) method in Beijing, China over a 4-yr

tions from aircraft (NCAR C-130 and NASA DC-8) and from the Tropospheric Emission Spectrometer (TES) satellite during the MegaCity Initiative: Local and Global Research

Size-resolved vertical aerosol number fluxes of particles in the diameter range 0.25–2.5 µm were measured with the eddy covariance method from a 53 m high tower over the Amazon