2018
DOI: 10.2514/1.c034412
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Local Solution to the Unsteady Stefan Problem for In-Flight Ice Accretion Modeling

Abstract: A new model for in-flight ice accretion is presented for both rime and glaze conditions. The model is based on the\ud local, exact solution of the unsteady Stefan problem for the temperature profiles within the ice layer in glaze\ud conditions. The new model moves from Myers’s formulation, and it includes an unsteady description of the heat\ud diffusion problem within the ice layer. Moreover, the local value of the air temperature outside the boundary layer is\ud used to compute convective heat fluxes, in plac… Show more

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Cited by 44 publications
(19 citation statements)
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“…Within each sub-domain, a one-dimensional phase-transition problem is solved (in the direction of the local surface normal). [6]. According to this reference, the 𝑄 bottom contribution, depending on the unsteady heat diffusion problem within the ice layer, can be expressed by means of a similarity variable…”
Section: B the Cloud Modelmentioning
confidence: 99%
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“…Within each sub-domain, a one-dimensional phase-transition problem is solved (in the direction of the local surface normal). [6]. According to this reference, the 𝑄 bottom contribution, depending on the unsteady heat diffusion problem within the ice layer, can be expressed by means of a similarity variable…”
Section: B the Cloud Modelmentioning
confidence: 99%
“…The reader is referred to the nomenclature section for the definition of each entry included in the aforementioned equations and to Ref. [6] for a comprehensive analysis of the accretion model.…”
Section: B the Cloud Modelmentioning
confidence: 99%
See 1 more Smart Citation
“…The model used in this work to capture the complex experimental ice shapes is the local exact solution of the unsteady Stefan problem for the temperature profiles within the ice layer in glaze conditions (Ref. 34). This model moves from Myers' formulation and includes an unsteady description of the heat diffusion problem within the ice layer and uses local values of the air temperature outside the boundary layer to compute the convective heat fluxes.…”
Section: Methodsmentioning
confidence: 99%
“…The PoliMIce software library provides state-of-the-art ice formation models [16]. The model used in this work to capture the complex experimental ice shapes is the local exact solution of the unsteady Stefan problem for the temperature profiles within the ice layer in glaze conditions [19]. Multi-step ice accretion simulations are performed at 5 second intervals to iteratively update the solution and account for unsteady ice accretion.…”
Section: D -Naca0012 Airfoilmentioning
confidence: 99%