07 Feb 2024
 | 07 Feb 2024
Status: a revised version of this preprint is currently under review for the journal ACP.

Quantifying the dust direct radiative effect in the Southwestern United States: findings from multiyear measurements

Alexandra Meiko Kuwano, Amato Evan, Blake Walkowiak, and Robert Frouin

Abstract. Mineral aerosols (i.e., dust) can affect climate and weather by absorbing and scattering shortwave (SW) and longwave (LW) radiation in the Earth’s atmosphere (the direct radiative effect). It is thought that the dust direct radiative effect is sufficiently strong that the presence of dust can significantly alter surface temperatures, static stability of the atmosphere, and the top of the atmosphere energy balance. Yet despite its importance, understanding of this parameter is so poor that, for example, the sign of the net direct radiative effect at top of the atmosphere is unconstrained, and thus it is unknown if changes in dust over time cool or warm Earth’s climate. Here we develop and apply new methods to estimate the SW direct effect via observations of aerosols and radiation made over a three-year period in a desert region of the southwestern United States. We generate region-specific dust optical properties via a novel data set of soil mineralogy from the Airborne Visible/Infrared Imaging Spectrometer (AVIRIS) instrument, which are then used to model the SW and LW dust direct radiative effect. From the observations and model output we find that the net dust direct radiative effect, on average, is −6 ± 1 and −2 ± 1 W m−2 at the surface and top of the atmosphere, respectively. Our results suggest that the magnitude of the SW component is about twice that in the LW, underscoring the importance of quantifying the iron oxide content of dust since these minerals strongly affect dust SW absorbtivity.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
Alexandra Meiko Kuwano, Amato Evan, Blake Walkowiak, and Robert Frouin

Status: final response (author comments only)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on acp-2024-1', Anonymous Referee #1, 26 Mar 2024
    • AC2: 'Reply on RC1', Alexandra Kuwano, 18 Jun 2024
  • RC2: 'Comment on acp-2024-1', Zhibo Zhang, 02 Apr 2024
    • AC3: 'Reply on RC2', Alexandra Kuwano, 18 Jun 2024
  • AC1: 'Comment on acp-2024-1', Alexandra Kuwano, 04 Jun 2024
Alexandra Meiko Kuwano, Amato Evan, Blake Walkowiak, and Robert Frouin
Alexandra Meiko Kuwano, Amato Evan, Blake Walkowiak, and Robert Frouin


Total article views: 533 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
408 92 33 533 23 20
  • HTML: 408
  • PDF: 92
  • XML: 33
  • Total: 533
  • BibTeX: 23
  • EndNote: 20
Views and downloads (calculated since 07 Feb 2024)
Cumulative views and downloads (calculated since 07 Feb 2024)

Viewed (geographical distribution)

Total article views: 513 (including HTML, PDF, and XML) Thereof 513 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
Latest update: 22 Jun 2024
Short summary
The dust direct radiative effect is highly uncertain. Here we used new measurements collected over three years and during dust storms at a field site in a desert region in southwestern United States to estimate the regional dust direct radiative effect. We also used novel soil mineralogy retrieved from an airborne spectrometer to estimate this parameter with model output. We find that, in this region, dust has a minimal net cooling effect on this region's climate.