@Article{MortariniDAOTSMABTGC:2022:CoStAn,
author = "Mortarini, Luca and Dias J{\'u}nior, Cl{\'e}o Q. and Acevedo,
Ot{\'a}vio Costa and Oliveira, Pablo E. S. and Tsokankunku,
Anywhere and S{\"o}rgel, Matthias and Manzi, Antonio Ocimar and
Ara{\'u}jo, Alessandro C. de and Brondani, Daiane V. and Toro,
Ivan Maur{\'{\i}}cio Cely and Giostra, Umberto and Cava,
Daniela",
affiliation = "{Consiglio Nazionale delle Ricerche (ISAC-CNR)} and {Instituto
Nacional de Pesquisas da Amaz{\^o}nia (INPA)} and {Instituto
Nacional de Pesquisas da Amaz{\^o}nia (INPA)} and {Universidade
Federal do Rio Grande do Norte (UFRN)} and {Max Planck Institute
for Chemistry} and {Max Planck Institute for Chemistry} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Embrapa
Amaz{\^o}nia Oriental} and {Instituto Nacional de Pesquisas da
Amaz{\^o}nia (INPA)} and {Universidade Federal de Santa Maria
(UFSM)} and {Universit{\`a} degli Studi di Urbino} and {Consiglio
Nazionale delle Ricerche (ISAC-CNR)}",
title = "Vertical propagation of submeso and coherent structure in a tall
and dense amazon forest in different stability conditions. PART
II: Coherent structures analysis",
journal = "Agricultural and Forest Meteorology",
year = "2022",
volume = "322",
pages = "e108993",
month = "July",
keywords = "Amazon forest, Canopy turbulence, Coherent structure, Mixing-layer
analogy, Roughness sublayer.",
abstract = "Observations of the vertical structure of the turbulent flow in
different stability regimes above and within the Amazon Forest at
the Amazon Tall Tower Observatory (ATTO) site have been presented
in Part I. Here, the influence of stability on the inception and
development of coherent structures is investigated. According to
the mixing-layer analogy the coherent vortices that dominate the
turbulent flows at the canopy-atmosphere interface are generated
by hydrodynamical instabilities triggered by an inflection in the
vertical profile of the mean wind speed at or near the canopy top.
The coherent motions time, Tpeak and separation length scale,
\Λ, depend on the shear length scale, Ls, close to the
canopy top. The present analysis studies the characteristics of
Ls, Tpeak and \Λ in the five stability regimes defined in
Part I. The behaviour of Ls with stability is evaluated and
parameterized. Ls increases with decreasing stability, presenting
two asymptotes for large unstable and stable stratification and a
linear behaviour close to neutral stratification. Coherent
structures and their timescale are detected with an original
method based on the autocorrelation functions of 5-min subsets of
turbulent quantities. The vertical time scale is larger in neutral
conditions and decreases for both increasing and decreasing
stability. At the canopy top the separation length scale presents
a linear dependence on Ls, whose slope is maximum in neutral
conditions and decreases departing from neutrality. An original
parameterization of the dependence of this slope on h/L, where h
is the canopy height and L is the Obukhov length, is shown.
Combining the parameterizations, the dependence of the separation
length scale is finally presented. \Λ has a maximum for
slightly unstable conditions, linearly decreases towards neutral
and weakly stable stratifications and then it tends to zero for
very intense unstable and stable stratifications.",
doi = "10.1016/j.agrformet.2022.108993",
url = "http://dx.doi.org/10.1016/j.agrformet.2022.108993",
issn = "0168-1923",
language = "en",
targetfile = "mortarini_2022_vertical.pdf",
urlaccessdate = "16 jun. 2024"
}