@Article{MortariniCaGiAcMaOlAn:2018:ObSuMo,
author = "Mortarini, Luca and Cava, D. and Giostra, U. and Acevedo, O. and
Martins, L. G. Nogueira and Oliveira, P. E. Soares de and Anfossi,
D.",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and Institute
of Atmospheric Sciences and Climate,Italy and {Universita degli
Studi di Urbino ‘Carlo Bo’} and {Universidade Federal de Santa
Maria (UFSM)} and {Universidade Federal de Santa Maria (UFSM)} and
{Universidade Federal de Santa Maria (UFSM)} and Institute of
Atmospheric Sciences and Climate,Italy",
title = "Observations of submeso motions and intermittent turbulent mixing
across a low level jet with a 132-m tower",
journal = "Quarterly Journal of the Royal Meteorological Society",
year = "2018",
volume = "144",
number = "710",
pages = "172--183",
month = "Jan.",
keywords = "meandering, gravity waves, low-wind conditions, atmospheric
turbulence, stable boundary layer, Eulerian autocorrelation
function, wavelet analysis, low-level jet.",
abstract = "The coexistence of wave-like submeso motions and anisotropic
intermittent turbulence in a night-time stable boundary layer is
investigated. Submeso motions of different characteristics and
amplitudes interact with each other. These interactions may lead
to intermittent turbulence production which alters the turbulent
structure of the stable boundary layer. On the other hand, the
production and transfer of turbulence affect the delicate balance
of submeso motions. In this work, sonic anemometer data collected
at 11 levels in southeastern Brazil have been used to study a case
of a nocturnal boundary layer at a coastal site. The absence of
forcing at the synoptic scale allows the development of a breeze
circulation on which a low-level jet of moderate intensity (4 m
s(-1)) and low height (about 50 m) takes place. The jet evolution
is coupled with dirty waves, while its full development is
associated with gravity waves driven by a strong vertical
temperature gradient. The layer centred at the low-level jet nose
is characterized by horizontal meandering and very weak turbulence
intensity. The air far below and above the low-level jet maximum
experiences bursts of significant increase of the turbulence
intensity, showing a three-layer structure. The oscillations of
the horizontal wind components exhibit the same frequency as the
temperature oscillations, suggesting that the presence of an
adequate temperature horizontal gradient is one of the fundamental
drivers of the meandering phenomenon. The considered night has
been studied by means of the Eulerian auto-correlation functions
for the detection of the meandering hours and their oscillation
time-scales, and by means of the continuous Morlet wavelet
function for the detection of the gravity waves and the
characterization of their spatial time-scales and temporal
evolution.",
doi = "10.1002/qj.3192",
url = "http://dx.doi.org/10.1002/qj.3192",
issn = "0035-9009",
language = "en",
targetfile = "mortarini_observations.pdf",
urlaccessdate = "27 abr. 2024"
}