We investigate the intermittent dynamics of momentum transport and its underlying time scales in the near-wall region of the neutrally stratified atmospheric boundary layer in the presence of a vegetation canopy. This is achieved through an empirical analysis of the persistence time scales (periods between successive zero-crossings) of momentum flux events, and their connection to the ejection-sweep cycle. Using high-frequency measurements from the GoAmazon campaign, spanning multiple heights within and above a dense canopy, the analysis suggests that, when the persistence time scales of momentum flux events from four different quadrants are separately normalized by (integral time scale of the vertical velocity), their distributions remain ...
We investigate the time intermittency of turbulent transport associated with the birth-death of self...
Turbulent transport of momentum and scalars over an urban canopy is investigated using the quadrant ...
Observations of the vertical structure of the turbulent flow in different stability regimes above an...
We investigate the intermittent dynamics of momentum transport and its underlying time scales in the...
We investigate the intermittent dynamics of momentum transport and its underlying time scales in the...
Using time series measurements of velocity, carbon dioxide and water vapour concentration, and tempe...
Biorthogonal decomposition (BOD) is used to detect and study synchronous coherent structures occurri...
The influence of coherent vortices on the turbulence structure above and below a dense plant canopy ...
Progress on many practical problems in eco-hydrology and eco-hydraulics are now requiring fundamenta...
How the presence of a canopy alters the clustering and the fine scale intermittency exponents and an...
© 2015 Elsevier B.V. Year round measurements of turbulence were taken at heights, above, below, and ...
We propose here a novel method of analysing turbulent momentum flux signals. The data for the analys...
Abstract. Dispersive flux terms are formed when the time-averaged mean momentum equation is spatiall...
Turbulent flow through and over vegetation continues to draw significant research attention given it...
To understand the basic characteristics of the observed S-shaped wind profile and the exponential fl...
We investigate the time intermittency of turbulent transport associated with the birth-death of self...
Turbulent transport of momentum and scalars over an urban canopy is investigated using the quadrant ...
Observations of the vertical structure of the turbulent flow in different stability regimes above an...
We investigate the intermittent dynamics of momentum transport and its underlying time scales in the...
We investigate the intermittent dynamics of momentum transport and its underlying time scales in the...
Using time series measurements of velocity, carbon dioxide and water vapour concentration, and tempe...
Biorthogonal decomposition (BOD) is used to detect and study synchronous coherent structures occurri...
The influence of coherent vortices on the turbulence structure above and below a dense plant canopy ...
Progress on many practical problems in eco-hydrology and eco-hydraulics are now requiring fundamenta...
How the presence of a canopy alters the clustering and the fine scale intermittency exponents and an...
© 2015 Elsevier B.V. Year round measurements of turbulence were taken at heights, above, below, and ...
We propose here a novel method of analysing turbulent momentum flux signals. The data for the analys...
Abstract. Dispersive flux terms are formed when the time-averaged mean momentum equation is spatiall...
Turbulent flow through and over vegetation continues to draw significant research attention given it...
To understand the basic characteristics of the observed S-shaped wind profile and the exponential fl...
We investigate the time intermittency of turbulent transport associated with the birth-death of self...
Turbulent transport of momentum and scalars over an urban canopy is investigated using the quadrant ...
Observations of the vertical structure of the turbulent flow in different stability regimes above an...