4.4 Article

Radar-Based Bayesian Estimation of Ice Crystal Growth Parameters within a Microphysical Model

Journal

JOURNAL OF THE ATMOSPHERIC SCIENCES
Volume 78, Issue 2, Pages 549-569

Publisher

AMER METEOROLOGICAL SOC
DOI: 10.1175/JAS-D-20-0134.1

Keywords

Cloud microphysics; Ice crystals; Radars; Radar observations; Bayesian methods; Cloud parameterizations

Funding

  1. DOE [DE-SC0018933]
  2. National Science Foundation
  3. U.S. Department of Energy (DOE) [DE-SC0018933] Funding Source: U.S. Department of Energy (DOE)

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The study explored the potential of polarimetric Doppler radar measurements to enhance predictions of ice microphysical processes within an idealized model-observational framework. A novel framework was developed to compare simulated and observed radar measurements, using Bayesian inference and a Markov chain Monte Carlo sampler to estimate the probability distribution of microphysical model parameters.
The potential for polarimetric Doppler radar measurements to improve predictions of ice microphysical processes within an idealized model-observational framework is examined. In an effort to more rigorously constrain ice growth processes (e.g., vapor deposition) with observations of natural clouds, a novel framework is developed to compare simulated and observed radar measurements, coupling a bulk adaptive-habit model of vapor growth to a polarimetric radar forward model. Bayesian inference on key microphysical model parameters is then used, via a Markov chain Monte Carlo sampler, to estimate the probability distribution of the model parameters. The statistical formalism of this method allows for robust estimates of the optimal parameter values, along with (non-Gaussian) estimates of their uncertainty. To demonstrate this framework, observations from Department of Energy radars in the Arctic during a case of pristine ice precipitation are used to constrain vapor deposition parameters in the adaptive habit model. The resulting parameter probability distributions provide physically plausible changes in ice particle density and aspect ratio during growth. A lack of direct constraint on the number concentration produces a range of possible mean particle sizes, with the mean size inversely correlated to number concentration. Consistency is found between the estimated inherent growth ratio and independent laboratory measurements, increasing confidence in the parameter PDFs and demonstrating the effectiveness of the radar measurements in constraining the parameters. The combined Doppler and polarimetric observations produce the highest-confidence estimates of the parameter PDFs, with the Doppler measurements providing a stronger constraint for this case.

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