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The development of near-vent volcanic ash cloud layers due to inhomogeneous atmospheric turbulence and relationship to wind shear. (arXiv:2101.01767v1 [physics.ao-ph]) http://arxiv.org/abs/2101.01767
The development of near-vent volcanic ash cloud layers due to inhomogeneous atmospheric turbulence and relationship to wind shear. (arXiv:2101.01767v1 [physics.ao-ph]) http://arxiv.org/abs/2101.01767