@Article{GamelinCarvKaya:2020:CoInEN,
author = "Gamelin, Brandi L. and Carvalho, Leila M. V. and Kayano, Mary
Toshie",
affiliation = "{University of California} and {University of California} and
{Instituto Nacional de Pesquisas Espaciais (INPE)}",
title = "The combined influence of ENSO and PDO on the spring UTLS ozone
variability in South America",
journal = "Climate Dynamics",
year = "2020",
volume = "55",
number = "5/6",
pages = "1539--1562",
month = "Sept.",
keywords = "ENSO, PDO, ENSO teleconnections, Upper troposphere-lower
stratosphere ozone, Rossby wave trains, South America.",
abstract = "Ozone in the upper troposphere-lower stratosphere (UTLS) is
primarily regulated by tropospheric dynamics. Understanding
mechanisms driving ozone variability at the UTLS is crucial to
evaluate the transport of mass to and from the lower stratosphere.
The El Nino-Southern Oscillation (ENSO) is the primary coupled
mode acting on interannual timescales modulating tropospheric
circulation worldwide. ENSO teleconnections can depend on the
phases of the Pacific Decadal Oscillation (PDO) and on the
characteristics of the warming over central and eastern tropical
Pacific. This study investigates the role of ENSO on UTLS ozone
variability with focus on South America and examines patterns of
teleconnections in the two recent warm (1980-1997) and cool
(1998-2012) PDO phases. The dominant mode of ozone variability is
identified by applying a principal component analysis (PCA) to
modern-era retrospective analysis for research and applications,
Version 2 (MERRA-2) ozone data from September-November (SON). SON
is the season with the largest UTLS ozone variance over South
America. The first mode resembles a Rossby wave train across South
America with spatial patterns dependent on PDO phase. We show that
the ENSO teleconnections and respective influences on SON UTLS
ozone are stronger during the cool PDO when ENSO and PDO are
mostly in phase. Additionally, the strength of the ENSO
teleconnection appears to depend on patterns of SST anomalies over
tropical Pacific. The decadal variability in the ENSO-PDO
relationships and teleconnections with the Southern Hemisphere
resulted in a shift in upper tropospheric circulation in tropical
and subtropical regions of South America.",
doi = "10.1007/s00382-020-05340-0",
url = "http://dx.doi.org/10.1007/s00382-020-05340-0",
issn = "0930-7575",
language = "en",
targetfile = "gamelin_combined.pdf",
urlaccessdate = "11 maio 2024"
}