@Book{LimaKuboSouz:2022:SeSuTe,
author = "Lima, Isabella Talamoni and Kubota, Paulo Yoshio and Souza, Dayana
Castilho de",
title = "The sea surface temperature diurnal cycle role in subseasonal and
seasonal meteorological systems",
publisher = "Instituto Nacional de Pesquisas Espaciais",
year = "2022",
address = "S{\~a}o Jos{\'e} dos Campos",
keywords = "sea surface temperature, diurnal cycle, ocean-atmosphere
interaction, subseasonal, seasonal.",
abstract = "The diurnal warming or Sea Surface Temperature (SST) diurnal cycle
is a mode of variation that has been receiving more attention
through the years. It plays an important role in the
ocean-atmosphere interaction because it modulates the air-sea
exchange at the interface, including energy (latent and sensible
heat), mass (water and trace gases) and momentum fluxes. Although
the global annual SST diurnal cycle amplitude (dSST) average is
0.1°C, over regions with strong incident radiation and weak winds
the dSST can reach values higher than 5°C. The diurnal energy is
stored in the Ocean Mixed Layer (OML) and interacts with daily,
intraseasonal and seasonal meteorological scales through SST
variability. However, the SST diurnal cycle is poorly represented
or parameterized in most numerical weather predictions and climate
studies. Therefore, this document explores the efforts made to
understand and represent the SST diurnal cycle and how it can
affect seasonal and subseasonal meteorological systems. RESUMO: O
aquecimento diurno ou ciclo diurno da Temperatura da
Superf{\'{\i}}cie do Mar (SST) {\'e} {\'e} um modo de
variabilidade que vem recebendo aten{\c{c}}{\~a}o ao longo dos
anos. Este ciclo exerce um papel importante na
intera{\c{c}}{\~a}o oceano-atmosfera porque modula as trocas
ar-mar que ocorrem na interface, incluindo os fluxos de energia
(calor sens{\'{\i}}vel e latente), de massa ({\'a}gua e gases
tra{\c{c}}o) e de momentum. Embora a m{\'e}dia global da
amplitude do ciclo diurno da SST (dSST) seja de O.1°C, em
regi{\~o}es com forte radia{\c{c}}{\~a}o incidente e ventos
fracos, a dSST pode atingir valores superiores a 5°C. A energia do
ciclo diurno {\'e} armazenada na Camada Limite Oce{\^a}nica
(OML) e interage com as escalas meteorol{\'o}gicas diurna,
subsazonal e sazonal por meio da variabilidade da SST. Apesar
disso, o ciclo diurno da SST ainda n{\~a}o {\'e} bem
representado ou parametrizado na maioria dos estudos
num{\'e}ricos de precis{\~a}o de tempo e clima. Portanto, este
documento buscou explorar os esfor{\c{c}}os feitos para entender
e representar o ciclo diurno da SST e como este pode afetar os
sistemas meteorol{\'o}gicos subsazonais e sazonais.",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)}",
label = "self-archiving-INPE-MCTIC-GOV-BR",
language = "en",
pages = "38",
ibi = "8JMKD3MGP3W34T/46TGJ8P",
url = "http://urlib.net/ibi/8JMKD3MGP3W34T/46TGJ8P",
targetfile = "publicacao.pdf",
urlaccessdate = "20 maio 2024"
}