Cited by 23Atmospheric chemistry and aerosolsAtmospheric aerosols and cloudsAtmospheric Ozone and Climate

Effect of aerosols and NO 2 concentration on ultraviolet actinic flux near Mexico City during MILAGRO: measurements and model calculations

Open access
Palancar, G. G., Lefer, B. L., Hall, S. R., Shaw, W. J., Corr, C. A., Herndon, S. C., Slusser, J. R., Madronich, S.·2013·Atmospheric Chemistry and Physics

Published version of a preprint

Abstract

Abstract. Urban air pollution absorbs and scatters solar ultraviolet (UV) radiation, and thus has a potentially large effect on tropospheric photochemical rates. We present the first detailed comparison between actinic fluxes (AF) in the wavelength range 330–420 nm measured in highly polluted conditions and simulated with the Tropospheric Ultraviolet-Visible (TUV) model. Measurements were made during the MILAGRO campaign near Mexico City in March 2006, at a ground-based station near Mexico City (the T1 supersite) and from the NSF/NCAR C-130 aircraft. At the surface, measured AF values are typically smaller than the model by up to 25% in the morning, 10% at noon, and 40% in the afternoon, for pollution-free and cloud-free conditions. When measurements of PBL height, NO2 concentration and aerosols optical properties are included in the model, the agreement improves to within ±10% in the morning and afternoon, and ±3% at noon. Based on daily averages, aerosols account for 68% and NO2 for 25% of AF reductions observed at the surface. Several overpasses from the C-130 aircraft provided the opportunity to examine the AF perturbations aloft, and also show better agreement with the model when aerosol and NO2 effects are included above and below the flight altitude. TUV model simulations show that the vertical structure of the actinic flux is sensitive to the choice of the aerosol single scattering albedo (SSA) at UV wavelengths. Typically, aerosols enhance AF above the PBL and reduce AF near the surface. However, for highly scattering aerosols (SSA > 0.95), enhancements can penetrate well into the PBL, while for strongly absorbing aerosols (SSA < 0.6) reductions in AF are computed in the free troposphere as well as in the PBL. Additional measurements of the SSA at these wavelengths are needed to better constrain the effect of aerosols on the vertical structure of the AF.

Integrity signals

Registry

Crossref · 10.5194/acp-13-1011-2013

Cites

56 of 56 references verified0 citation errors · 0 not checkable

Statistics

Recomputing p-values needs the paper’s full text.

Claims the paper makes

We couldn’t retrieve this paper’s full text, so its claims and self-check weren’t run. The registry and citation checks still apply.

Claims other papers make about this one

Each is checked against this paper’s own text: does it say what the citing paper says it does?

  • In CESM2(WACCM6), photolysis rates are calculated using lookup tables that account for the overhead ozone column and clouds but exclude the effects of aerosols, thereby reducing the effect SAI aerosols could have on tropospheric photochemistry and ozone.

    “in CESM2(WACCM6) photolysis rates are calculated using lookup tables, taking into account the overhead ozone column and clouds but excluding the effects of aerosols, thereby reducing the effect SAI aerosols could have on tropospheric photochemistry and ozone.”

Cites

Flagged first, then by citations

Cited by

Sorted by citations

Authors
Palancar, G. G., Lefer, B. L., Hall, S. R., Shaw, W. J., Corr, C. A., Herndon, S. C., Slusser, J. R., & Madronich, S.
Affiliations
  • NSF National Center for Atmospheric Research (US)
  • University of Houston (US)
  • Pacific Northwest National Laboratory (US)
  • University of New Hampshire (US)
  • Aerodyne Research (US)
  • Colorado State University (US)
Venue
Atmospheric Chemistry and Physics
Published
2013-01-24
Volume
13
Issue
2
Pages
1011-1022
ISSN
  • 1680-7316 (ISSN-L)
  • 1680-7324
OpenAlex
W1977567291
Cited by
23
References
56
Citations by year
2026: 1 · 2024: 1 · 2021: 5 · 2020: 1 · 2019: 2 · 2018: 5 · 2017: 1 · 2015: 2 · 2014: 2 · 2013: 1 · 2012: 1
FWCI
1.09
Type
journal article
Language
en
Open access
Locations
  • Atmospheric chemistry and physics (publishedVersion, cc-by)
  • Americanae (AECID Library) (submittedVersion, cc-by-nc-sa)
  • DOAJ (DOAJ: Directory of Open Access Journals) (submittedVersion, cc-by-sa)
  • LA Referencia (Red Federada de Repositorios Institucionales de Publicaciones Científicas) (submittedVersion, cc-by-nc-sa)
Funders
  • National Science Foundation (0511911)
  • U.S. Department of Agriculture
  • National Center for Atmospheric Research
  • Consejo Nacional de Investigaciones Científicas y Técnicas
  • Cooperative State Research, Education, and Extension Service
Topics
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Atmospheric chemistry and aerosols
  • Physical Sciences › Environmental Science › Global and Planetary Change › Atmospheric aerosols and clouds
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Atmospheric Ozone and Climate
Keywords
actinic flux, nitrogen dioxide, urban air pollution, tropospheric photochemistry, single scattering albedo, boundary layer height, TUV model, Mexico City, MILAGRO campaign, airborne measurements, aerosol optical properties

About these checks

Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.

Statistics and arithmetic are recomputed, not judged.

Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.

What counts as a claim ›How we measure confidence ›How we check this ›

Are you an author, or do you see a problem with this page? Request a review