The atmospheric boundary layer (ABL) defines the volume of air adjacent to the Earth's
surface for the dilution of heat, moisture, and trace substances. Quantitative knowledge on …

Diurnal mountain wind systems are local thermally driven wind systems that form over
mountainous terrain and are produced by the buoyancy effects associated with the diurnal …

Laboratory studies have established a number of chemical pathways by which nitrogen
oxides (NO x) affect atmospheric organic aerosol (OA) production. However, these effects …

Mountainous terrain exerts an important influence on the Earth's atmosphere and affects
atmospheric transport and mixing at a wide range of temporal and spatial scales. The …

The atmospheric boundary layer mediates the exchange of energy, matter, and momentum
between the land surface and the free troposphere, integrating a range of physical …

Peatland drainage is an important driver of global soil carbon loss and carbon dioxide (CO2)
emissions. Restoration of peatlands by reflooding reverses CO2 losses at the cost of …

We investigated the effect of land use on differences in air temperature. We based our
analysis on a decade of weather and energy flux measurements, collected over two …

Mixing layer height (h) is an important parameter for understanding the transport process in
the troposphere, air pollution, weather and climate change. Many methods have been …

The spatiotemporal evolution of the atmospheric boundary layer (ABL), in a narrow, highly
complex terrain located in the Colombian Andes, is studied using radiosondes and remote …

Significant progress has been made in reducing emissions of air pollutants in the San
Joaquin Valley in California. Nevertheless, from May to October, the valley still experiences …