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On the Formation of the Low-Level Jet over Texas
Monthly Weather Review, 1980Abstract The low-level jet (LLJ) in the winter half-year originates as a south wind over the high plains of Colorado. Kansas, western Oklahoma and West Texas. After formation, the LLJ spreads horizontally and upstream toward the Gulf of Mexico. The air in the LLJ becomes humid when the entrance to the jet moves to the Gulf.
Dus̆an Djurić, Michel S. Damiani
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The Intra‐Americas Sea Low‐level Jet
Annals of the New York Academy of Sciences, 2008A relevant climate feature of the Intra‐Americas Sea (IAS) is the low‐level jet (IALLJ) dominating the IAS circulation, both in summer and winter; and yet it is practically unknown with regard to its nature, structure, interactions with mid‐latitude and tropical phenomena, and its role in regional weather and climate.
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A nocturnal low level jet during PUKK
Boundary-Layer Meteorology, 1985A nocturnal low-level jet characterized by a distinct inertial oscillation lasting from around sunset until sunrise the next day was observed during the coastal experiment PUKK. The phenomenon appeared over an area of at least 40 km in diameter; it thus had a mesoscale extension.
Helmut Kraus +2 more
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Raptor responses to low-level jet aircraft and sonic booms
Environmental Pollution, 1991We estimated effects of low-level military jet aircraft and mid- to high-altitude sonic booms (actual and simulated) on nesting peregrine falcons (Falco peregrinus) and seven other raptors by observing their responses to test stimuli, determining nesting success for the test year, and evaluating site reoccupancy rates for the year following the tests ...
D H, Ellis, C H, Ellis, D P, Mindell
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The Low-Level Jet as a Western Boundary Current
Monthly Weather Review, 1976Abstract The low-level jet which flows across the equator and up the Somali coast is considered as a western boundary current of the East African mountain chain. The jet is assumed to be forced by the low-level divergence in the subtropical high pressure belt of the Southern Hemisphere and convergence in the monsoon trough.
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Observations of Low-level Jet Physics and Impacts
2020The Great Plains low-level jet (LLJ) is a planetary boundary layer phenomenon of strong winds spanning thousands of square kilometers. These LLJs are primarily nocturnal, and an event?s lifetime can exceed 12 hours. LLJ wind speeds can reach 30 m/s within the lowest several hundred meters of the atmosphere. The formation mechanisms of the strongest and
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Importance of Low-Level Jets to Climate: A Review
Journal of Climate, 1996Abstract Low-level jets (LLJs) occur frequently in many parts of the world. These low-level wind speed maxima are important for both the horizontal and vertical fluxes of temperature and moisture and have been found to be associated with the development and evolution of deep convection.
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Low-level Jet at White Sands Missile Range
Journal of Applied Meteorology, 1966Abstract Wind data collected at White Sands Missile Range, New Mexico, frequently show a sharp maximum in the wind speed profile below 3000 ft. This low-level maximum is often supergeostrophic and associated with large values of wind shear in the lower levels.
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Conversion of bio-jet fuel from palm kernel oil and its blending effect with jet A-1 fuel
Energy Conversion and Management, 2021Wei-Hsin Chen +2 more
exaly
Reanalysis: Climatology of the Low Level Jet
Bulletin of the American Meteorological Society, 2019openaire +1 more source