Two-Step Polishing Technique for Flat and Smooth Copper Substrates by Electrochemical and Chemical Etching. [PDF]
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An Oxygenating Video Laryngoscope Blade With an Integrated Lens‑Clearing Gas Jet for Management of the Soiled Airway During Tracheal Intubation: Concept and Design Considerations. [PDF]
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Investigation of Vortex-Driven Mixing in Hydrogen-Ammonia Low Pressure Direct Injection. [PDF]
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Machine learning-assisted evolutionary optimization of hole quality and surface integrity in abrasive waterjet drilling of polycarbonate. [PDF]
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Effect of the Injector Pressure-Building Process on Dynamic Gas Flow Characteristics of a Highly Turbulent Underexpanded Hydrogen Jet from a Single-Hole Cylindrical Injector. [PDF]
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The impact of London on a low-level jet
2021<p>The low-level jet (LLJ) is an important phenomenon that can affect (and is affected by) the turbulence in the nocturnal urban boundary layer (UBL). We investigate the interaction of a regional LLJ with the UBL during a 2-day period over London.
Aristofanis Tsiringakis +3 more
openaire +1 more source
The Use of Low-Level Jets by Migrating Birds
Naturwissenschaften, 1999Birds flying at high altitudes have occasionally been observed above mountain areas and the open sea. For the first time the regular occurrence of migrating birds flying within a low-level jet at heights of 5000 to almost 9000 m asl. have now been verified by radar above the Negev desert in southern Israel.
F, Liechti, E, Schaller
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A LOW-LEVEL JET IN THE TROPICS
Monthly Weather Review, 1971Abstract A temporary mesoscale network of pilot balloon stations on a tropical island (Barbados, West Indies) revealed the existence of a low-level jet at 700 m above mean sea level, with a maximum wind near 40 m/s and a duration of at least 2 hr. The phenomenon appears to be associated with the Venturi effect produced in the low levels by a traveling ...
R. L. DeSOUZA +4 more
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Kinematics of the Low-Level Jet
Journal of Applied Meteorology, 1968Abstract Winds and vertical velocities are examined in ten southerly low-level jets and then averaged in coordinate systems centered on the jet. The jet at 0600 CST is strongly supergeostrophic but is reflected in both geostrophic and ageostrophic components of the wind. Air is typically rising downstream from the wind maximum and sinking just upstream
W. D. Bonner, S. Esbensen, R. Greenberg
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Features of the Caribbean low level jet
International Journal of Climatology, 2007AbstractThe Caribbean Low Level Jet (CLLJ) is shown to be a real and dominant climatological feature of the early summer Caribbean climate. It manifests as an intensification in the trade winds in the western Caribbean basin (70°W–80°W) with an east‐west axis along 15°N.
Felicia S. Whyte +3 more
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