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remote sensing Communication On the Potential of Flaming Hotspot Detection at Night via Multiband Visible/Near-Infrared Imaging

Record‐Low Arctic Stratospheric Ozone in 2020: MLS Observations of Chemical Processes and Comparisons With Previous Extreme Winters

Seasonal and Regional Signatures of ENSO in Upper Tropospheric Jet Characteristics from Reanalyses

Manney, G. L., M. I. Hegglin, and Z. Lawrence (2021), Seasonal and Regional Signatures of ENSO in Upper Tropospheric Jet Characteristics from Reanalyses, J. Climate, 34, 9181-9200, doi:10.1175/JCLI-D-20-0947.1.

A Moments View of Climatology and Variability of the Asian Summer Monsoon Anticyclone

Manney, G. L., et al. (2021), A Moments View of Climatology and Variability of the Asian Summer Monsoon Anticyclone, J. Climate, 34, 7821-7841, doi:10.1175/JCLI-D-20-0729.1.

Introduction to Special Collection "The Exceptional Arctic Stratospheric Polar Vortex in 2019/2020: Causes and Consequences”

Manney, G. L., et al. (2022), Introduction to Special Collection "The Exceptional Arctic Stratospheric Polar Vortex in 2019/2020: Causes and Consequences”, J. Geophys. Res., 127, The Exceptional Arctic Stratos, doi:https://doi.org/10.1029/2022JD037381.

What's in a Name? On the Use and Significance of the Term “Polar Vortex”

Manney, G. L., et al. (2023), What's in a Name? On the Use and Significance of the Term “Polar Vortex”, Geophys. Res. Lett., 49, doi:https://doi.org/10.1029/2021GL097617.

Signatures of Anomalous Transport in the 2019/2020 Arctic Stratospheric Polar Vortex

Manney, G. L., et al. (2023), Signatures of Anomalous Transport in the 2019/2020 Arctic Stratospheric Polar Vortex, J. Geophys. Res., 127, e2022JD037407, doi:10.1029/2022JD037407.

Siege in the southern stratosphere: Hunga Tonga-Hunga Ha'apai water vapor excluded from the 2022 Antarctic polar vortex

North Atlantic Ocean SST-gradient-driven variations in aerosol and cloud evolution along Lagrangian cold-air outbreak trajectories

Linking marine phytoplankton emissions, meteorological processes, and downwind particle properties with FLEXPART

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