The aerodynamic roughness length is a crucial parameter that controls surface variables
including the horizontal wind, surface temperature, and heat fluxes. Despite its importance …

Comprehensive characterization of turbulent fluxes and land‐atmosphere interactions at a
semi‐arid region in the Deccan Plateau of peninsular India is presented using 2‐year eddy …

Using observational data acquired during the Monsoon Trough Boundary Layer Experiment
(MONTBLEX‐90), the drag coefficient CD is estimated over two land stations, Jodhpur (arid …

An attempt has been made here to examine the contrasting variations in mean surface layer
parameters including surface fluxes, and in surface layer stability between the convective …

Observational data in the atmosphere indicate that conventionally defined drag and heat
transfer coefficients increase rapidly as wind speed falls. It is shown here that, at sufficiently …

For the first time, the exchange coefficient of heat CH has been estimated from eddy
correlation of velocity and virtual temperature fluctuations using sonic anemometer …

Abstract Kaiga, in the Western Ghats region, has a hilly topography and dense forest
canopy. In this study, the sensitivity of surface roughness length (zo) on the boundary layer …

The aerodynamic roughness length (z_ 0)(z 0) is estimated here for four locations,
Bangalore, Ranchi, Hyderabad and Tirunelveli of the Indian region, using …

The aerodynamic drag coefficient (CD) is conjectured to change (or remains almost uniform)
with the horizontal wind speed (U) over a flexible (or fixed) surface element, which is …

Abstract Structure of the atmospheric surface layer on diurnal and seasonal time scales has
been studied for ten categories of land surface patterns of the Indian region by making full …