TY - JOUR
T1 - Tropical tropospheric ozone trends (1998 to 2023)
T2 - New perspectives from SHADOZ, IAGOS and OMI/MLS observations
AU - Thompson, Anne M.
AU - Stauffer, Ryan M.
AU - Kollonige, Debra E.
AU - Ziemke, Jerald R.
AU - Johnson, Bryan J.
AU - Morris, Gary A.
AU - Cullis, Patrick
AU - Cazorla, María
AU - Diaz, Jorge Andres
AU - Piters, Ankie
AU - Nedeljkovic, Igor
AU - Warsodikromo, Truus
AU - Raimundo Silva, Francisco
AU - Northam, E. Thomas
AU - Benjamin, Patrick
AU - Mkololo, Thumeka
AU - Machinini, Tshidi
AU - Félix, Christian
AU - Romanens, Gonzague
AU - Nyadida, Syprose
AU - Brioude, Jérôme
AU - Evan, Stéphanie
AU - Metzger, Jean Marc
AU - Dindang, Ambun
AU - Mahat, Yuzaimi B.
AU - Sammathuria, Mohan Kumar
AU - Zakaria, Norazura Binti
AU - Komala, Ninong
AU - Ogino, Shin Ya
AU - Quyen, Nguyen Thi
AU - Mani, Francis S.
AU - Vuiyasawa, Miriama
AU - Nardini, David
AU - Martinsen, Matthew
AU - Kuniyuki, Darryl T.
AU - Müller, Katrin
AU - Wolff, Pawel
AU - Sauvage, Bastien
N1 - Publisher Copyright:
© 2025 Anne M. Thompson et al.
PY - 2025/12/19
Y1 - 2025/12/19
N2 - Tropospheric ozone trends are important indicators of climate forcing and surface pollution, yet relevant satellite observations are too uncertain for assessments. The assessment project TOAR-II has used multi-instrument, ground-based data for global trends over 2000-2022 (Van Malderen et al., 2025a, b). For the tropics, trends are derived from SHADOZ ozonesonde profiles (Thompson et al., 2021, "T21"; Stauffer et al., 2024) or combinations of satellite, SHADOZ and IAGOS aircraft measurements (Gaudel et al., 2024). We extend T21 that covered 1998-2019, analyzing SHADOZ data at five sites with a Multiple Linear Regression (MLR) model for 1998-2023 and reporting trends for two free-tropospheric (FT) segments, the lowermost stratosphere and the total tropospheric column (TrCOsonde). Trends for the Aura period, 2005-2023, are computed from OMI/MLS TrCOsatellite. We find the following: Extending SHADOZ analyses 4 years shows little change from T21; TrCOsonde trends are small (0.5-1 DU/decade) except over SE Asia. Annual trends for TrCOsonde and OMI/MLS TrCOsatellite agree within uncertainties at four of five sites, with the largest differences at Samoa. Sensitivity tests show the following: (a) Adding thousands of FT IAGOS profiles to SHADOZ yields little change in trends; SHADOZ sampling is sufficient. (b) Quantile Regression (QR) and MLR median trends are both near zero, but QR captures extremes (5th percentile, 95th percentile) with changes up to ±1 DU/decade (p< 0.10). (c) Twelve-year analyses for trends lead to uncertainty changes too large for an assessment. This study and Van Malderen et al. (2025a, b) provide the most reliable TOAR-II trends to date: over the past ∼ 25 years, tropical FT ozone changes have been modest, ∼ (-3-+3) %/decade, except over SE Asia.
AB - Tropospheric ozone trends are important indicators of climate forcing and surface pollution, yet relevant satellite observations are too uncertain for assessments. The assessment project TOAR-II has used multi-instrument, ground-based data for global trends over 2000-2022 (Van Malderen et al., 2025a, b). For the tropics, trends are derived from SHADOZ ozonesonde profiles (Thompson et al., 2021, "T21"; Stauffer et al., 2024) or combinations of satellite, SHADOZ and IAGOS aircraft measurements (Gaudel et al., 2024). We extend T21 that covered 1998-2019, analyzing SHADOZ data at five sites with a Multiple Linear Regression (MLR) model for 1998-2023 and reporting trends for two free-tropospheric (FT) segments, the lowermost stratosphere and the total tropospheric column (TrCOsonde). Trends for the Aura period, 2005-2023, are computed from OMI/MLS TrCOsatellite. We find the following: Extending SHADOZ analyses 4 years shows little change from T21; TrCOsonde trends are small (0.5-1 DU/decade) except over SE Asia. Annual trends for TrCOsonde and OMI/MLS TrCOsatellite agree within uncertainties at four of five sites, with the largest differences at Samoa. Sensitivity tests show the following: (a) Adding thousands of FT IAGOS profiles to SHADOZ yields little change in trends; SHADOZ sampling is sufficient. (b) Quantile Regression (QR) and MLR median trends are both near zero, but QR captures extremes (5th percentile, 95th percentile) with changes up to ±1 DU/decade (p< 0.10). (c) Twelve-year analyses for trends lead to uncertainty changes too large for an assessment. This study and Van Malderen et al. (2025a, b) provide the most reliable TOAR-II trends to date: over the past ∼ 25 years, tropical FT ozone changes have been modest, ∼ (-3-+3) %/decade, except over SE Asia.
UR - https://www.scopus.com/pages/publications/105025530074
U2 - 10.5194/acp-25-18475-2025
DO - 10.5194/acp-25-18475-2025
M3 - Artículo
AN - SCOPUS:105025530074
SN - 1680-7316
VL - 25
SP - 18475
EP - 18507
JO - Atmospheric Chemistry and Physics
JF - Atmospheric Chemistry and Physics
IS - 24
ER -