Dust in the Critical Zone: North American case studies

Authors

J. Brahney, Utah State University
R. C. Heindel, Kenyon College
T. E. Gill, The University of Texas at El Paso
G. Carling, The College of Physical and Mathematical Sciences
J. M. González-Olalla, Utah State University
J. Hand, Cooperative Institute for Research in the Atmosphere
D. V. Mallia, University of Utah, College of Mines and Earth Sciences
J. S. Munroe, Middlebury College
K. Perry, University of Utah, College of Mines and Earth Sciences
A. L. Putman, United States Geological Survey Central Region
S. M. Skiles, The University of Utah
B. R. Adams, Ira A. Fulton College of Engineering
Z. Aanderud, Brigham Young University
S. Aarons, University of California, San Diego
D. Aguirre, Utah State University
K. Ardon-Dryer, Texas Tech University
M. B. Blakowski, Utah State University
J. M. Creamean, Walter Scott, Jr. College of Engineering
D. Fernandez, University of Utah, College of Mines and Earth Sciences
H. Foroutan, Virginia Tech College of Engineering
C. Gaston, University of Miami
M. Hahnenberger, Salt Lake Community College
S. Hoch, University of Utah, College of Mines and Earth Sciences
D. K. Jones, United States Geological Survey Central Region
K. E. Kelly, John and Marcia Price College of Engineering
O. I. Lang, The University of Utah
J. LeMonte, The College of Physical and Mathematical Sciences
R. Reynolds, College of Science and Engineering
R. P. Singh, Chapman University
M. Sweeney, University of South Dakota
T. Merrill, University of Utah, College of Mines and Earth Sciences

Document Type

Article

Publication Date

11-1-2024

Publication Title

Earth Science Reviews

Keywords

Aerosols, Critical zone, Dust, Earth systems, Particulate matter

Abstract

The dust cycle facilitates the exchange of particles among Earth's major systems, enabling dust to traverse ecosystems, cross geographic boundaries, and even move uphill against the natural flow of gravity. Dust in the atmosphere is composed of a complex and ever-changing mixture that reflects the evolving human footprint on the landscape. The emission, transport, and deposition of dust interacts with and connects Critical Zone processes at all spatial and temporal scales. Landscape properties, land use, and climatic factors influence the wind erosion of soil and nutrient loss, which alters the long-term ecological dynamics at erosional locations. Once in the atmosphere, dust particles influence the amount of solar radiation reaching Earth, and interact with longwave (terrestrial) radiation, with cascading effects on the climate system. Finally, the wet and dry deposition of particles influences ecosystem structure, composition, and function over both short and long-term scales. Tracking dust particles from source to sink relies on monitoring and measurement of the geochemical composition and size distribution of the particles, space-borne and ground-based remote sensing, and dust modeling. Dust is linked to human systems via land use and policies that contribute to dust emissions and the health-related consequences of particulate loads and composition. Despite the significant influence dust has in shaping coupled natural-human systems, it has not been considered a key component of the Critical Zone. Here, we demonstrate that dust particles should be included as a key component of the Critical Zone by outlining how dust interacts with and shapes Earth System processes from generation, through transport, to deposition. We synthesize current understanding from global research and identify critical data and knowledge gaps while showcasing case studies from North America.

Volume

258

ISSN

00128252

DOI

10.1016/j.earscirev.2024.104942

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