@Article{SchmenglerCoAcPuDeMaMe:2015:CoMiLe,
author = "Schmengler, Moacir and Costa, Felipe Denardin and Acevedo,
Ot{\'a}vio Costa and Puhales, Franciano S. and Demarco, Giuliano
and Martins, Lu{\'{\i}}s Gustavo Nogueira and Medeiros, Luiz
Eduardo",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Universidade Federal do Pampa} and {Universidade Federal de Santa
Maria (USFM)} and {Universidade Federal de Santa Maria (USFM)} and
{Universidade Federal de Santa Maria (USFM)} and {Universidade
Federal de Santa Maria (USFM)} and {Universidade Federal de Santa
Maria (USFM)}",
title = "Comparison of mixing length formulations in a single-column model
simulation for a very stable site",
journal = "American Journal of Environmental Engineering",
year = "2015",
volume = "5",
number = "1A",
pages = "106--118",
keywords = "Very Stable Boundary Layer, Atmospheric Modeling, Mixing Length
Formulations.",
abstract = "Reproducing the behavior of the mean variables that control the
nocturnal atmospheric flow under very stable conditions is a very
difficult task for atmospheric models. To understand the role of
the surface scheme, turbulence scheme and radiation scheme on the
performance of a single column model, its predictions are compared
to observations collected at a very stable site located in
deforested region in Amazon. The surface scheme takes on
consideration the rapid changes in the surface energy budget
caused by the presence of a vegetated layer over the soil. The
turbulence scheme uses four different formulations for the mixing
length. Two of them allow the existence of turbulence over the
critical Richardson number, while the other two restrict
dramatically the turbulence activity in those situations. The
radiative scheme considers a clear sky condition, and evaluates
the radiative flux divergence between 3 levels within the vertical
domain: near the surface, at the domain top, and at the middle
point between them. The predictions of all mixing length
formulations are very similar to the observed data near the
surface, indicating that in this region the surface plays a
crucial role. At upper levels the most turbulent formulations lead
to better results. This is a consequence of atmospheric decoupling
when the turbulence is completely suppressed, which leads to
colder results near the surface and warmer results aloft. The
radiative scheme reproduces quite well the temperature decay above
the boundary layer for all cases, in spite of its simplicity. On
the other hand, the comparison between modeled and observed
humidity profiles shows that it is necessary to improve the model
by including a more complete scheme for humidity and by adding a
advection scheme to it.",
doi = "10.5923/s.ajee.201501.14",
url = "http://dx.doi.org/10.5923/s.ajee.201501.14",
issn = "2166-4633 and 2166-465X",
label = "lattes: 7237707809890993 1 SchmenglerCoAcPuDeMaMe:2015:CoMiLe",
language = "en",
urlaccessdate = "27 abr. 2024"
}