Keratin recovered from animal‐hair textile waste is fractionated and blended with cellulose to produce continuously spun hybrid fibers. Selecting the high‐molecular‐weight keratin fraction enables 30 wt.% keratin incorporation while maintaining high strength in dry and wet states.
Mian Zhai +6 more
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Frequency-Dependent Responses of Extensometers to Atmospheric Loading: Evidence from Geodynamical Observatory Jingyuan in the NE Margin of the Tibetan Plateau. [PDF]
Yang J, Yang X.
europepmc +1 more source
Greenland Emissions Contribute to Black Carbon Aerosols in the Arctic Marine Boundary Layer. [PDF]
Teng X +13 more
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GNSS/eLoran Fusion-Based RAIM for Satellite-Deficient Environments. [PDF]
Li J, Wu H.
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Emerging nitrogen-driven urban atmosphere control on aerosol iron dissolution for biogeochemical cycles. [PDF]
Wang G +14 more
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Optimized Design and Radiation Error Correction of a Naturally Ventilated Air Temperature Sensor for Atmospheric Environmental Monitoring. [PDF]
Jin W +5 more
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Climate and plant traits drive a cross-continental imbalance in atmospheric Hg uptake. [PDF]
Jia L +13 more
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Observation of Atmospheric Neutrinos [PDF]
In 1998, the Super-Kamiokande discovered neutrino oscillation using atmospheric neutrino anomalies. It was the first direct evidence of neutrino mass and the first phenomenon to be discovered beyond the standard model of particle physics. Recently, more precise measurements of neutrino oscillation parameters using atmospheric neutrinos have been ...
Yusuke Koshio
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Atmospheric processes and observations
Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences, 2003The central role of the atmosphere in abrupt climate change is proposed and discussed. This discussion is given in the context of the poleward transport of energy in the climate system and of climate variability and change. A number of examples based on observational and model data are used to illustrate the ideas.
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Atmospheric glories: simulations and observations
Applied Optics, 2005Mie theory can be used to provide full-color simulations of atmospheric glories. Comparison of such simulations with images of real glories suggests that most glories are caused by spherical water droplets with radii between 4 and 25 microm. This paper also examines the appearance of glories taking into account the size of the droplets and the width of
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