Results 241 to 250 of about 94,167 (304)

Modelling of sea surface coupled losses in surface duct propagation

OCEANS 2022 - Chennai, 2022
Neethu S, Satheesh Kumar S
exaly   +2 more sources

Full-Coupled Convolutional Transformer for Surface-Based Duct Refractivity Inversion

open access: yesRemote Sensing, 2022
This is source code of paper: Full-coupled convolutional Transformer for surface-based duct refractivity ...
Jiajing Wu   +2 more
exaly   +2 more sources

Effectiveness of duct cleaning methods on newly installed duct surfaces

Indoor Air, 2003
Two kinds of air duct cleaning methods, mechanical brushing with different brushes and compressed air cleaning, were compared in the laboratory and in newly built buildings. The ducts were contaminated either with test dust or with dust originated from a construction site.
R. Holopainen   +5 more
openaire   +3 more sources

Attenuation in surface ducts

The Journal of the Acoustical Society of America, 1978
Two surface duct propagation experiments are examined in which absorption and diffraction appear to be the dominant attenuation mechanisms. The absence of an excess diffusion loss suggests that little or no internal scatter occurs in a mixed layer. This result is consistent with the internal wave scatter hypothesis.
R. H. Mellen, D. G. Browning
openaire   +1 more source

Sialography and Surface Anatomy of the Parotid Duct

Archives of Otolaryngology - Head and Neck Surgery, 1960
The many variations in shape and extent of the parotid gland are well known. The parotid gland is larger than indicated in textbooks. 14 Not only does this structure vary in different persons, but also on the two sides of the same person. 36 Hetzar's 15 finding of differences of the parotid glands in the two sexes and in persons of different ...
H. OPPENHEIM, M. WING
openaire   +2 more sources

Mixed layers and surface ducts

The Journal of the Acoustical Society of America, 2021
The upper ocean is strongly effected by the sun and the wind. In an idealized view, this leads to a warm mixed layer with a nearly constant temperature and salinity. Then, the increase in pressure with depth causes an increase of about 1.7 m/s in sound speed for every 100 m in depth (i.e., a gradient of 0.017/s). This gradient forms an acoustic surface
openaire   +1 more source

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