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Tropical isoprene variability differs across three regions

Aerial overhead view of a dense tropical rainforest canopy with lush green vegetation and scattered lighter-colored tree crowns, creating a natural patchwork pattern typical of tropical jungle landscape.
Research area:Atmospheric sciencesAtmospheric ScienceClimate variability and models

What the study found

Tropical isoprene column variability showed different responses to El Niño-Southern Oscillation across Amazonia, the Maritime Continent, and equatorial Africa. The authors describe Amazonia as emissions-controlled, the Maritime Continent as chemistry-controlled, and equatorial Africa as an intermediate regime.

Why the authors say this matters

The study suggests that comparing these regional regimes can help explain interactions between volatile organic compound (VOC) emissions and nitrogen oxides (NOx) sources over tropical areas with few in-situ observations. The authors also highlight oil palm plantations in the Maritime Continent as an area where isoprene and soil NOx fluxes are co-located.

What the researchers tested

The researchers used isoprene retrievals from the Cross-track infrared sounder (CrIS) to monitor global isoprene column variability. They compared those retrievals with temperature, precipitation, soil moisture, and formaldehyde retrievals across Amazonia, the Maritime Continent, and equatorial Africa.

What worked and what didn't

In Amazonia, isoprene column variability correlated with temperature, which the authors interpret as evidence that emissions drive the variability. In the Maritime Continent, isoprene columns were strongly correlated with precipitation and soil moisture and anti-correlated with formaldehyde, which the authors say suggests modulation by non-anthropogenic NOx emissions from soil and biomass burning, although convection and lightning NOx may also play a role if lofted isoprene flux is large enough. In equatorial Africa, both biomass burning and temperature explained isoprene variability during different periods.

What to keep in mind

The abstract does not provide detailed limitations beyond noting that the regions differ in dynamic temperature and oxidant range. Some suggested controls, such as convection, lightning NOx, and the role of lofted isoprene flux, are presented as possible contributors rather than settled explanations.

Key points

  • CrIS isoprene retrievals were used to track global isoprene column variability.
  • Amazonia showed correlations with temperature, which the authors interpret as emissions-controlled variability.
  • The Maritime Continent showed links with precipitation, soil moisture, and an anti-correlation with formaldehyde.
  • The authors suggest chemistry-related controls in the Maritime Continent, including soil and biomass burning NOx.
  • Equatorial Africa appeared to be an intermediate regime with both biomass burning and temperature contributing at different times.

Disclosure

Research title:
Tropical isoprene variability differs across three regions
Authors:
James Young Suk Yoon, Kelley C. Wells, Dylan B. Millet, Christian Frankenberg, S. Sanghavi, Abigail L. S. Swann, Joel A. Thornton, Alexander J. Turner
Institutions:
University of Washington, University of Minnesota, California Institute of Technology, Jet Propulsion Laboratory
Publication date:
2026-04-02
OpenAlex record:
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AI provenance: This post was generated by OpenAI. The original authors did not write or review this post.