An aircraft case study of the spatial transition from closed to open mesoscale cellular convection over the Southeast Pacific

Simulated aerosol size distributions are in reasonable agreement with obser- vations in the marine boundary layer and in the free troposphere, while the model underestimates

Based on a simple dilution ap- proach for the plume we found the chemical lifetime (defined as time when differences between plume and background air are reduced to 5% or less) of

The model of the boundary layer with two sharp boundaries used in this study leads to a somewhat larger (compared to models of the medium with a smooth transition layer,

Most of the trajectories that reached the boundary layer travelled from the Western Pacific, ∼ 20–40 ◦ E of Borneo, suggesting that measurements of VSLS in the TTL over Borneo might

As this equatorward expansion of the open- closed ®eld line boundary continued, enhanced electron and ion temperatures were seen above the ESR, in response to the precipitation

Following recent observations of molecular io- dine (I 2 ) in the coastal marine boundary layer (MBL) (Saiz- Lopez and Plane, 2004), it has become important to deter- mine the

We investigated the spatial structure of tropical forest vegetation and its relationship to the hydrological network and associated topographic structure across spatial scales

Box model simulations of an uplifting and adiabatically cooling cloud of aerosol have been performed in order to study the transition between cirrus formation dominated by