atmospheric boundary layer उदाहरण वाक्य

Businger has been described as one of the first to recognize the scientific and practical importance of the atmospheric boundary layer ( ABL ) and worked on the development of the sonic anemometer.
During its existence, Boundary-Layer Meteorology has become the primary medium for the publication of theoretical, numerical and experimental studies of the atmospheric boundary layer over both land and sea surfaces.
Ridge A is a low ridge of ice and has been estimated to have very low disturbances to visibility, such as thick atmospheric boundary layer, amount of water vapour and numerous others.
The lowest and turbulent part of the atmosphere, the atmospheric boundary layer, is not a closed box, but constantly brings in dry air from higher up in the atmosphere towards the surface.
He joined the British Meteorological Office in 1939 and was asked to study turbulent diffusion in the atmospheric boundary layer ( the first few hundred metres of atmosphere above the earth's surface ).

Carson joined the UK Meteorological Office in 1969, following his Ph . D from the Department of Applied Mathematics, University of Liverpool, working on the structure and evolution of the atmospheric boundary layer.
He was educated at the University of East Anglia ( BSc ) and the University of Southampton ( PhD ), where his thesis was on numerical modelling of the atmospheric boundary layer over the ocean.
The wind profile of the atmospheric boundary layer ( surface to around 2000 metres ) is generally logarithmic in nature and is best approximated using the log wind profile equation that accounts for surface roughness and atmospheric stability.
Phenomena of climatological interest include the atmospheric boundary layer, latent ), interactions between the atmosphere and the oceans and land surface ( particularly vegetation, land use and topography ), and the chemical and physical composition of the atmosphere.
Mesoscale meteorology is the study of atmospheric phenomena that has horizontal scales ranging from 1 km to 1000 km and a vertical scale that starts at the Earth's surface and includes the atmospheric boundary layer, troposphere, tropopause, and the lower section of the stratosphere.