4.7 Article

Aerosol-Ice Formation Closure: A Southern Great Plains Field Campaign

Journal

BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY
Volume 102, Issue 10, Pages E1952-E1971

Publisher

AMER METEOROLOGICAL SOC
DOI: 10.1175/BAMS-D-20-0151.1

Keywords

Aerosols; Cloud microphysics; Glaciation; Aerosol indirect effect; Aerosol-cloud interaction; particulates

Funding

  1. Atmospheric System Research Program
  2. Atmospheric Radiation Measurement Program - U.S. Department of Energy (DOE), Office of Science, Office of Biological and Environmental Research (OBER), Climate and Environmental Sciences Division (CESD) [DE-SC0020006]
  3. NASA Radiation Science, and Modeling, Analysis and Prediction Programs
  4. National Science Foundation [CHE1554941, CBET1804737]
  5. NSF [006784]
  6. U.S. DOE Office of Science, OBER [DE-SC0018979]
  7. OBER at Pacific Northwest National Laboratory (PNNL)
  8. Office of Science, Office of Basic Energy Sciences, of the U.S. DOE [DE-AC02-05CH11231]
  9. [DE-SC0021034]
  10. [DE-SC0018929]
  11. [DE-SC0018948]
  12. [DE-SC0020510]
  13. [DE-SC0019192]
  14. [DE-SC0016237]
  15. U.S. Department of Energy (DOE) [DE-SC0018979, DE-SC0018929, DE-SC0020006] Funding Source: U.S. Department of Energy (DOE)

Ask authors/readers for more resources

The prediction of ice formation in clouds presents a significant challenge in atmospheric sciences, particularly the uncertainty in deriving INP number concentrations in cloud-resolving and climate models. The closure pilot study aims to evaluate the level of parameter details and measurement strategies needed to achieve aerosol-ice formation closure, with a focus on guiding immersion freezing schemes in models and identifying causes for INP prediction biases in climate models.
Prediction of ice formation in clouds presents one of the grand challenges in the atmospheric sciences. Immersion freezing initiated by ice-nucleating particles (INPs) is the dominant pathway of primary ice crystal formation in mixed-phase clouds, where supercooled water droplets and ice crystals coexist, with important implications for the hydrological cycle and climate. However, derivation of INP number concentrations from an ambient aerosol population in cloud-resolving and climate models remains highly uncertain. We conducted an aerosol-ice formation closure pilot study using a field-observational approach to evaluate the predictive capability of immersion freezing INPs. The closure study relies on collocated measurements of the ambient size-resolved and single-particle composition and INP number concentrations. The acquired particle data serve as input in several immersion freezing parameterizations, which are employed in cloud-resolving and climate models, for prediction of INP number concentrations. We discuss in detail one closure case study in which a front passed through the measurement site, resulting in a change of ambient particle and INP populations. We achieved closure in some circumstances within uncertainties, but we emphasize the need for freezing parameterization of potentially missing INP types and evaluation of the choice of parameterization to be employed. Overall, this closure pilot study aims to assess the level of parameter details and measurement strategies needed to achieve aerosol-ice formation closure. The closure approach is designed to accurately guide immersion freezing schemes in models, and ultimately identify the leading causes for climate model bias in INP predictions.

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