Effect of discontinuities in surface catalytic activity on laminar heat transfer in arc-heated nitrogen streams
Discontinuity effects in surface catalytic activity on laminar heat transfer in arc heated nitrogen streams
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Discontinuity effects in surface catalytic activity on laminar heat transfer in arc heated nitrogen streams
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Flow of unsteady compressible boundary layer over semiinfinite flat plate whose temperature exceeds free stream temperature
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Irregular variations of earth rotation velocity explained by action of solar corpuscular streams on magnetosphere
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Methods of calculating short shells and reinforced shells, and experiments on self-oscillations of cylindrical panels in supersonic gas stream
Steady geomagnetic micropulsations and solar corpuscular streams
Free-stream interference effects on effectiveness of control jets near wing tip of VTOL aircraft model
Unsteady incompressible laminar forced convection around stagnation point due to arbitrary timewise- variant free stream velocity, considering skin friction and heat transfer
Output of an eddy-resolving model of the North Atlantic is diagnosed in the vicinity of the Gulf Stream (GA), using quasigeostrophic potential voracity (QGPV), Ertel's potential voracity (PV), and particle trajectories. Time series of QGPV show strong input of QGPV by the GS in the top 100 m of the model ocean.
During 1992-3 as the Ulysses spacecraft passed in and out of the southern high speed solar wind stream, the Solar Wind Ion Spectrometer, SWICS made continuous composition and temperature measurements of all major solar wind ions.
Satellite synthetic-aperture radar (SAR) Interferometry is employed to map the hinge line, or limit of tidal flexing, of Rutford Ice Stream and Carlson Inlet, Antarctica, and detect its migration between 1992 and 1996. The hinge line is mapped using a model fit from an elastic beam theory.
We have examined the ISEE-3 distant tail data during three intense (Dst< -100(sub n)T) magnetic storms and have identified the tail response to high speed solar wind streams, interplanetary magnetic clouds, and near-Earth storms. The three storms have a peak Dst ranging from -150 to -220 nT, and occur on Jan. 9, Feb. 4, and Aug. 8, 1993.
This paper compares the performances of two different types of data-derived symbol synchronizers, namely, Filter and Square (FS) and Digital Data Transition Tracking Loop (DTTL), in the presence of unbalanced data streams.
Ocean backscatter signatures were measured by the Jet Propulsion Laboratory airborne NUSCAT K(sub u)-band scatterometer across the Gulf Stream sea surface temperature front. The measurements were made during the Surface Wave Dynamics Experiment (SWADE) off the coast of Virginia and Maryland in the winter of 1991.