4.7 Article

Mineral dust cycle in the Multiscale Online Nonhydrostatic AtmospheRe CHemistry model (MONARCH) Version 2.0

期刊

GEOSCIENTIFIC MODEL DEVELOPMENT
卷 14, 期 10, 页码 6403-6444

出版社

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/gmd-14-6403-2021

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资金

  1. European Union [690462]
  2. Helmholtz Association's Initiative and Networking Fund [VH-NG-1533]
  3. European Research Council (FRAGMENT) [773051]
  4. AXA Research Fund
  5. Spanish Ministry of Science, Innovation and Universities [CGL2017-88911-R]
  6. EU H2020 project FORCES [821205, CMUG-CCI3-TECHPROP]
  7. European Space Agency (ESA) - FORMAS
  8. DLR
  9. BMWFW
  10. MINECO
  11. ANR (FR)
  12. NASA Modeling, Analysis and Prediction Program [NNG14HH42I]
  13. National Science Foundation (NSF) [1552519, 1856389]
  14. Army Research Office [W911NF-20-2-0150]
  15. Columbia University Earth Institute
  16. NASA [80NSSC19K1346]
  17. Future Investigators in NASA Earth and Space Science and Technology (FINESST) program
  18. European Research Council (ERC) [773051] Funding Source: European Research Council (ERC)
  19. Div Atmospheric & Geospace Sciences
  20. Directorate For Geosciences [1856389] Funding Source: National Science Foundation

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In this study, the dust module in the MONARCH model was upgraded with a focus on dust emission, lower boundary conditions, and dust-radiation interactions. Different parameterizations were used to model the global dust cycle, and the simulations were evaluated against observational data. Key dust parameters and their effects on radiative forcing were determined, showing important differences between different configurations.
We present the dust module in the Multiscale Online Non-hydrostatic AtmospheRe CHemistry model (MONARCH) version 2.0, a chemical weather prediction system that can be used for regional and global modeling at a range of resolutions. The representations of dust processes in MONARCH were upgraded with a focus on dust emission (emission parameterizations, entrainment thresholds, considerations of soil moisture and surface cover), lower boundary conditions (roughness, potential dust sources), and dust-radiation interactions. MONARCH now allows modeling of global and regional mineral dust cycles using fundamentally different paradigms, ranging from strongly simplified to physics-based parameterizations. We present a detailed description of these updates along with four global benchmark simulations, which use conceptually different dust emission parameterizations, and we evaluate the simulations against observations of dust optical depth. We determine key dust parameters, such as global annual emission/deposition flux, dust loading, dust optical depth, mass-extinction efficiency, single-scattering albedo, and direct radiative effects. For dust-particle diameters up to 20 mu m, the total annual dust emission and deposition fluxes obtained with our four experiments range between about 3500 and 6000 Tg, which largely depend upon differences in the emitted size distribution. Considering ellipsoidal particle shapes and dust refractive indices that account for size-resolved mineralogy, we estimate the global total (longwave and shortwave) dust direct radiative effect (DRE) at the surface to range between about -0.90 and -0.63 W m(-2) and at the top of the atmosphere between -0.20 and -0.28 W m(-2). Our evaluation demonstrates that MONARCH is able to reproduce key features of the spatiotemporal variability of the global dust cycle with important and insightful differences between the different configurations.

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