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Turbulent boundary layers up to Reθ=2500 studied through simulation and experiment
Direct numerical simulations (DNSs) and experiments of a spatially developing zero-pressure-gradient turbulent boundary layer are presented up to Reynolds number Re-theta=2500, based on momentum thExpand
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A mammalian fossil from the Dingqing Formation in the Lunpola Basin, northern Tibet, and its relevance to age and paleo-altimetry
The distal extremity of a rhinocerotid humerus from the upper part of the Dingqing Formation at the Lunbori locality in Baingoin County, northern Tibet, is the first mammalian fossil found inExpand
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Simulations of Spatially Evolving Turbulent Boundary Layers up to Reθ = 4300
A well-resolved large-eddy simulation (LES) of a spatially developing turbulent boundary layer under zero pressure gradient up to comparably high Reynolds numbers (Reθ = 4300) is performed. TheExpand
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Chiral magnetic effect in ZrTe5
The chiral magnetic effect is the generation of electric current induced by chirality imbalance in the presence of magnetic field. It is a macroscopic manifestation of the quantum anomaly inExpand
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Complete boundary element formulation for normal and tangential contact problems
The boundary element method as a numerical tool in contact mechanics is widely used and allows for surface roughness to be investigated with very fine grids. However, for every two grid points,Expand
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DNS of a spatially developing turbulent boundary layer with passive scalar transport
Abstract A direct numerical simulation (DNS) of a spatially developing turbulent boundary layer over a flat plate under zero pressure gradient (ZPG) has been carried out. The evolution of severalExpand
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Jet angular correlation in vector-boson fusion processes at hadron colliders
Higgs boson and massive-graviton productions in association with two jets via vector-boson fusion (VBF) processes and their decays into a vector-boson pair at hadron colliders are studied. TheyExpand
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Rare backflow and extreme wall-normal velocity fluctuations in near-wall turbulence
Rare negative streamwise velocities and extreme wall-normal velocity fluctuations near the wall are investigated for turbulent channel flow at a series of Reynolds numbers based on friction velocityExpand
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What drives the observed variability of HCN in the troposphere and lower stratosphere
Abstract. We use the GEOS-Chem global 3-D chemistry transport model to investigate the relative importance of chemical and physical processes that determine observed variability of hydrogen cyanideExpand
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PMSE-observations with the EISCAT VHF and UHF-radars: Statistical properties
Abstract Observations of polar mesosphere summer echoes (PMSE) have been carried out with the EISCAT VHF radar during five summer seasons between 2003 and 2007 as well as with the EISCAT UHF radar inExpand
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