497 research outputs found

    Super-resolving multi-photon interferences with independent light sources

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    We propose to use multi-photon interferences from statistically independent light sources in combination with linear optical detection techniques to enhance the resolution in imaging. Experimental results with up to five independent thermal light sources confirm this approach to improve the spatial resolution. Since no involved quantum state preparation or detection is required the experiment can be considered an extension of the Hanbury Brown and Twiss experiment for spatial intensity correlations of order N>2

    Isotope shifts and hyperfine structure of the Fe I 372 nm resonance line

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    We report measurements of the isotope shifts of the 3d64s2a5D4−3d64s4pz5F5o3d^64s^2 a ^5D_4 - 3d^64s4p z ^5F_5^o Fe I resonance line at 372 nm between all four stable isotopes 54^{54}Fe, 56^{56}Fe, 57^{57}Fe, and 58^{58}Fe, as well as the complete hyperfine structure of that line for 57^{57}Fe, the only stable isotope having a non-zero nuclear spin. The field and specific mass shift coefficients of the transition have been derived from the data, as well as the experimental value for the hyperfine structure magnetic dipole coupling constant AA of the excited state of the transition in 57^{57}Fe: A(3d64s4pz5F5o)=81.69(86)A(3d^64s4p z ^5F_5^o) = 81.69(86) MHz. The measurements were done by means of Doppler-free laser saturated-absorption spectroscopy in a Fe-Ar hollow cathode using both natural and enriched iron samples. The measured isotope shifts and hyperfine constants are reported with uncertainties at the percent level.Comment: 5 pages, 5 figure

    Numerical study of rainbows and glories in water-drop clouds

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    In this paper we study scattering phase functions in water-drop clouds for various distributions of droplet size and various conditions of glory, rainbow and corona formation, and discuss the hypothesis proposed by A. N. Nevzorov that a considerable amount of water in cold clouds can exist in a specific phase state with the refractive index ≈ 1.8 (so called A-water). Polarization and angular distributions are studied by the Monte Carlo method for radiation reflected by cloud layers with drops of water or hypothetical A-water taking into account multiple scattering. Computational results make it possible to develop procedures for analysis of microphysical structure of clouds and confirmation or disproof of the existence of A-water

    Plans to eradicate invasive mammals on an island inhabited by humans and domestic animals (Corvo, Azores, Portugal)

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    Oppel, S., Beaven, B.M., Bolton, M., Bodey, T.W., Geraldes, P., Oliveira, N., Hervias, S., Henriques, A., Silva, C
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