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- W2079543089 abstract "Abstract The standard picture of atmospheric dynamics is that of an isotropic two-dimensional large scale and an isotropic three-dimensional small scale, the two separated by a dimensional transition called the “mesoscale gap.” Evidence now suggests that, on the contrary, atmospheric fields, while strongly anisotropic, are nonetheless scale invariant right through the mesoscale. Using visible and infrared satellite cloud images and the formalism of generalized scale invariance (GSI), the authors attempt to quantify the anisotropy for cloud radiance fields in the range 1–1000 km. To do this, the statistical translational invariance of the fields is exploited by studying the anisotropic scaling of lines of constant Fourier amplitude. This allows the investigation of the change in shape and orientation of average structures with scale. For the three texturally—and meteorologically—very different images analyzed, three different generators of anisotropy are found that generally reproduce well the Fourier spac..." @default.
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- W2079543089 date "1993-02-01" @default.
- W2079543089 modified "2023-10-17" @default.
- W2079543089 title "Differential Rotation and Cloud Texture: Analysis Using Generalized Scale Invariance" @default.
- W2079543089 doi "https://doi.org/10.1175/1520-0469(1993)050<0538:dracta>2.0.co;2" @default.
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