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Chinese Journal of Physics, 2019
zbMATH Open Web Interface contents unavailable due to conflicting licenses.
Alatas, Husin, Tsauqi, Angga K.
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zbMATH Open Web Interface contents unavailable due to conflicting licenses.
Alatas, Husin, Tsauqi, Angga K.
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Acta Crystallographica Section A, 1976
A crystal structure in P{\bar 1} consisting of N identical atoms in the whole unit cell is fixed, and the four non-negative numbers R1, R2, R12/2, R_{1{\bar 2}/2} are also specified. The random variables (vectors) h, k are assumed to be uniformaly and independently distributed in the regions of reciprocal space defined by |Eh| = R1, |Ek| = R2, |E(h + k)
E. A. Green, H. Hauptman
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A crystal structure in P{\bar 1} consisting of N identical atoms in the whole unit cell is fixed, and the four non-negative numbers R1, R2, R12/2, R_{1{\bar 2}/2} are also specified. The random variables (vectors) h, k are assumed to be uniformaly and independently distributed in the regions of reciprocal space defined by |Eh| = R1, |Ek| = R2, |E(h + k)
E. A. Green, H. Hauptman
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Journal of the Optical Society of America, 1979
Expressions are derived for higher-order skewness and excess coefficients using central moments and cumulants up to 8th order. These coefficients are then calculated for three probability distributions: (1) Log-normal, (2) Rice-Nakagami, and (3) Gamma distributions.
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Expressions are derived for higher-order skewness and excess coefficients using central moments and cumulants up to 8th order. These coefficients are then calculated for three probability distributions: (1) Log-normal, (2) Rice-Nakagami, and (3) Gamma distributions.
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Journal of the Atmospheric Sciences, 1982
Abstract This paper aims to develop and test a parameterization scheme for partial cloudiness, to be used in the framework of higher-order models of the turbulent planetary boundary layer. The proposed scheme is designed to be general enough and fairly accurate, although slightly at the expense of simplicity.
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Abstract This paper aims to develop and test a parameterization scheme for partial cloudiness, to be used in the framework of higher-order models of the turbulent planetary boundary layer. The proposed scheme is designed to be general enough and fairly accurate, although slightly at the expense of simplicity.
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Stochastic Environmental Research and Risk Assessment, 2011
Forecasting of extreme events and phenomena that respond to non-Gaussian heavy-tailed distributions (e.g., extreme environmental events, rock permeability, rock fracture intensity, earthquake magnitudes) is essential to environmental and geoscience risk analysis.
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Forecasting of extreme events and phenomena that respond to non-Gaussian heavy-tailed distributions (e.g., extreme environmental events, rock permeability, rock fracture intensity, earthquake magnitudes) is essential to environmental and geoscience risk analysis.
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Field-strength probability distributions and higher-order squeezing
Physical Review A, 1990openaire +2 more sources
Reduced order and surrogate models for gravitational waves
Living Reviews in Relativity, 2022Manuel Tiglio, Aaron Villanueva
exaly
High-order fully actuated system approaches: Part III. Robust control and high-order backstepping
International Journal of Systems Science, 2021Guang-Ren Duan
exaly
Review of second-order models for adsorption systems
Journal of Hazardous Materials, 2006Yuh-Shan Ho
exaly