Summertime Diurnal Variability of Formaldehyde Over the Contiguous United States: Constraints From Pandonia Global Network

Abstract The diurnal cycle of Formaldehyde (HCHO) provide critical insights into tropospheric photochemistry. Here we use tropospheric HCHO retrievals from the Pandonia Global Network (PGN), combined with NASA's GEOS Composition Forecast (GEOS‐CF) model to understand the diurnal variation of summertime HCHO across the contiguous US. While PGN HCHO tropospheric column (HCHO trop ) shows a weak diurnal cycle in most regions, a distinct midday peak is found at the urban sites of Southern US (mainly in Houston), likely driven by highly reactive VOC emissions. For the vertical profile of HCHO mixing ratio within the Planetary Boundary Layer (PBL), PGN shows a significant decrease from 0.5 to 2 km while GEOS‐CF exhibits an excessively well‐mixed vertical shape. This discrepancy in HCHO profile leads to an overestimated HCHO trop in GEOS‐CF in Northeast Coastal US and Southeast US. These findings offer valuable insights for interpreting geostationary satellite observations and understanding model biases in surface ozone (O 3 ).

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Publication Details

Journal
Geophysical Research Letters
Published
2025-10-13
DOI
https://doi.org/10.1029/2025gl116033
Citations
2
Primary Topic
Atmospheric chemistry and aerosols
Type
article
Field-Weighted Citation Impact
2.60

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article

Summertime Diurnal Variability of Formaldehyde Over the Contiguous United States: Constraints From Pandonia Global Network

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2 citations
Geophysical Research Letters
Atmospheric chemistry and aerosols
2.60
article

Summertime Diurnal Variability of Formaldehyde Over the Contiguous United States: Constraints From Pandonia Global Network

Jingqiu Mao, Tianlang Zhao, Alexander Cede, Elena Spinei, K. Emma Knowland, Jennifer Kaiser, Viral P. Shah, Martin Tiefengraber, Xiaoyi Zhao, Manuel Gebetsberger, Thomas Frost Hanisco, Apoorva Pandey
article en
2 citations

Abstract

Abstract The diurnal cycle of Formaldehyde (HCHO) provide critical insights into tropospheric photochemistry. Here we use tropospheric HCHO retrievals from the Pandonia Global Network (PGN), combined with NASA's GEOS Composition Forecast (GEOS‐CF) model to understand the diurnal variation of summertime HCHO across the contiguous US. While PGN HCHO tropospheric column (HCHO trop ) shows a weak diurnal cycle in most regions, a distinct midday peak is found at the urban sites of Southern US (mainly in Houston), likely driven by highly reactive VOC emissions. For the vertical profile of HCHO mixing ratio within the Planetary Boundary Layer (PBL), PGN shows a significant decrease from 0.5 to 2 km while GEOS‐CF exhibits an excessively well‐mixed vertical shape. This discrepancy in HCHO profile leads to an overestimated HCHO trop in GEOS‐CF in Northeast Coastal US and Southeast US. These findings offer valuable insights for interpreting geostationary satellite observations and understanding model biases in surface ozone (O 3 ).

Geophysical Research LettersVol. 52(20)
Goddard Space Flight Center (US), Georgia Institute of Technology (US), Environment and Climate Change Canada (CA), University of Alaska Fairbanks (US), University of Maryland, Baltimore County (US), Morgan State University (US)
National Aeronautics and Space Administration, Nuclear Safety and Security Commission, Langley Research Center, Office of Experimental Program to Stimulate Competitive Research
Openalex Percentile: Top 9%
Atmospheric chemistry and aerosols
2.60
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