Low Tropospheric Ozone Over the Indo‐Pacific Warm Pool Related to Non‐Electrified Convection

Low Tropospheric Ozone Over the Indo‐Pacific Warm Pool Related to Non‐Electrified Convection

Abstract Lightning is the most important source of nitric oxide (NO) in the tropical upper troposphere and controls the formation of tropospheric ozone (O3). It is associated with deep convection and occurs mostly over continents. The Chemistry of the Atmosphere Field Experiment in the Pacific (CAFE...

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Bibliographic Details
Main Authors: Clara M. Nussbaumer, Andrea Pozzer, Michael Hewson, Linda Ort, Bianca Krumm, Joseph Byron, Jonathan Williams, Philipp Joppe, Florian Obersteiner, Andreas Zahn, Jos Lelieveld, Horst Fischer
Format: Article
Language:English
Published: Wiley 2025-03-01
Series:Geophysical Research Letters
Subjects:
tropospheric ozone
deep convection
lightning
Indo‐Pacific warm Pool
Australia
in situ observations
Online Access:https://doi.org/10.1029/2024GL112788
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https://doi.org/10.1029/2024GL112788

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