Behavior of topside and bottomside spread F at equatorial latitudes
Diurnal variation of topside and bottomside spread-F and geomagnetic effects from Alouette I ionograms
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Diurnal variation of topside and bottomside spread-F and geomagnetic effects from Alouette I ionograms
Occurrence frequency patterns of topside spread-F on Alouette satellite ionograms, discussing radio propagation, magnetic irregularities, electron density-induced refraction, etc
Equatorial spread-F and tropical disturbances, supplying data on typhoon, geomagnetic activity and atmospheric pressure waves
Radio star Cassiopeia A scintillations and spread-F in auroral zone
In a computational model of spreading depression (SD), ionic movement through a neuronal syncytium of cells connected by gap junctions is described electrodiffusively. Simulations predict that SD will not occur unless cells are allowed to expand in response to osmotic pressure gradients and K+ is allowed to move through gap junctions. SD waves of [K+]out approximately 25 to approximately 60 mM moving at approximately 2 to approximately 18 mm/min are predicted over the range of parametric values reported in gray matter, with extracellular space decreasing up to approximately 50%. Predicted waveform shape is qualitatively similar to laboratory reports. The delayed-rectifier, NMDA, BK, and Na+ currents are predicted to facilitate SD, while SK and A-type K+ currents and glial activity impede SD. These predictions are consonant with recent findings that gap junction poisons block SD and support the theories that cytosolic diffusion via gap junctions and osmotic forces are important mechanisms underlying SD.
Since Chaney’s report, the range of global warming projections in response to a doubling of CO2—from 1.5 °C to 4.5 °C or greater—remains largely unscathed by the onslaught of new scientific insights. Conventional thinking regards inter-model differences in climate feedbacks as the sole cause of the warming projection spread (WPS). Our findings shed new light on this issue indicating that climate feedbacks inherit diversity from the model control climate, besides the models’ intrinsic climate feedback diversity that is independent of the control climate state. Regulated by the control climate ice coverage, models with greater (lesser) ice coverage generally possess a colder (warmer) and drier (moister) climate, exhibit a stronger (weaker) ice-albedo feedback, and experience greater (weaker) warming. The water vapor feedback also inherits diversity from the control climate but in an opposite way: a colder (warmer) climate generally possesses a weaker (stronger) water vapor feedback, yielding a weaker (stronger) warming. These inherited traits influence the warming response in opposing manners, resulting in a weaker correlation between the WPS and control climate diversity. Our study indicates that a better understanding of the diversity amongst climate model mean states may help to narrow down the range of global warming projections.
Chemical and fluid dynamic parameters effecting the flame spreading process downstream from a bluff-body flame holder
Stability of liquid layer of uniform thickness spread over rigid circular cylinder subjected to lateral accelerations
Spreading resistance as function of geometry and frequency in semiconductor diodes
Flame spreading over surface of igniting composite solid propellant constituents
Limits of head wave amplitudes for short spreads from charges, blasting caps, and 45-kilogram weight drops
Diurnal behavior of topside and bottomside spread F at equatorial latitudes and association with geomagnetic activity
Flame spreading over igniting surface of double base propellants in high pressure quiescent environment
Effects of aspect ratio on spreading of semi-confined jets formed by round and sharp edged nozzle profiles
Rotating interferometer measuring spread and coherence ratio of scattered radio wave
Field equations for spreading resistance of variable capacitance diode and point contact variable resistance diode derived in terms of frequency, material characteristics and physical parameters
Flame spreading over igniting solid propellant surface in high pressure oxygen-inert environment
Midlatitude topside spread F studied by Alouette 1 ionograms recorded at Woomera