@Article{StefanelloRBRFFBHATRD:2023:ImAtBo,
author = "Stefanello, Michel and Rosa, Cinara Ewerling da and Bresciani,
Caroline and Reis, Nicolle Cordero Sim{\~o}es dos and Facco,
Douglas Stefanello and Ferraz, Simone E. Teleginski and Boiaski,
Nathalie Tissot and Herdies, Dirceu Luis and Acevedo, Ot{\'a}vio
and Tirabassi, Tiziano and Roberti, D{\'e}bora Regina and
Degrazia, Gerv{\'a}sio Annes",
affiliation = "{Universidade Federal de Santa Maria (UFSM)} and {Instituto
Federal Farroupilha} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Universidade Federal de Santa Maria (UFSM)}
and {Universidade Federal do Rio Grande do Sul (UFRGS)} and
{Universidade Federal de Santa Maria (UFSM)} and {Universidade
Federal de Santa Maria (UFSM)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Universidade Federal de Santa
Maria (UFSM)} and {Universidade Federal de Santa Maria (UFSM)} and
{Universidade Federal de Santa Maria (UFSM)} and {Universidade
Federal de Santa Maria (UFSM)}",
title = "Spatial–temporal analysis of a summer heat wave associated with
downslope flows in southern Brazil: implications in the
atmospheric boundary layer",
journal = "Atmosphere",
year = "2023",
volume = "14",
number = "1",
pages = "e64",
month = "Jan.",
keywords = "atmospheric boundary layer, downslope winds, heat wave, regional
meteorology, topography effect.",
abstract = "This study investigates a summer heat wave (HW) associated with
downslope winds (DWs) affecting the central region of the state of
Rio Grande do Sul (RS), Brazil. The temporal evolution of both
phenomena is analyzed in the atmospheric boundary layer (ABL)
using a combination of micrometeorological and rawinsonde data.
For spatial characterization, ERA-5 reanalysis data are used. The
HW covered a large area in southern Brazil, Argentina, and
Paraguay. The main features of the HW were locally enhanced in the
central region of RS by the development of DWs. The establishment
of DWs near the surface depends on the dynamics of the ABL and
local topographic features. The results showed that DWs that
occurred during the HW contributed to the extreme temperatures and
were associated with strong northerly winds, low relative
humidity, and a drop in the dew points. Together, these extreme
events influenced the turbulent and mean flow patterns of the ABL.
The increase in turbulent activity associated with the warming of
the ABL favored enhanced growth of morning ABL, while at night the
simultaneous effects of radiative and turbulence cooling inhibited
the formation of a strong stable ABL. The analysis highlights the
complex interplay of synoptic and local factors associated with
DWs and HW.",
doi = "10.3390/atmos14010064",
url = "http://dx.doi.org/10.3390/atmos14010064",
issn = "2073-4433",
language = "en",
targetfile = "atmosphere-14-00064.pdf",
urlaccessdate = "01 maio 2024"
}