902,721 research outputs found
The cooling-off effect of price limits in the Chinese stock markets
In this paper, we investigate the cooling-off effect (opposite to the magnet
effect) from two aspects. Firstly, from the viewpoint of dynamics, we study the
existence of the cooling-off effect by following the dynamical evolution of
some financial variables over a period of time before the stock price hits its
limit. Secondly, from the probability perspective, we investigate, with the
logit model, the existence of the cooling-off effect through analyzing the
high-frequency data of all A-share common stocks traded on the Shanghai Stock
Exchange and the Shenzhen Stock Exchange from 2000 to 2011 and inspecting the
trading period from the opening phase prior to the moment that the stock price
hits its limits. A comparison is made of the properties between up-limit hits
and down-limit hits, and the possible difference will also be compared between
bullish and bearish market state by dividing the whole period into three
alternating bullish periods and three bearish periods. We find that the
cooling-off effect emerges for both up-limit hits and down-limit hits, and the
cooling-off effect of the down-limit hits is stronger than that of the up-limit
hits. The difference of the cooling-off effect between bullish period and
bearish period is quite modest. Moreover, we examine the sub-optimal orders
effect, and infer that the professional individual investors and institutional
investors play a positive role in the cooling-off effects. All these findings
indicate that the price limit trading rule exerts a positive effect on
maintaining the stability of the Chinese stock markets
New physical principles of contact thermoelectric cooling
We suggest a new approach to the theory of the contact thermoelectric cooling
(Peltier effect). The metal-metal, metal-n-type semiconductor, metal-p-type
semiconductor, p-n junction contacts are analyzed. Both degenerate and
non-degenerate electron and hole gases are considered. The role of
recombination in the contact cooling effect is discussed by the first time.Comment: 8 pages, 8 figures, revtex
Modeling radiation in particle clouds: On the importance of inter-particle radiation for pulverized solid fuel combustion
The importance of inter-particle radiation for clusters of gray and diffuse
particles is investigated. The radiative cooling of each individual particle is
found to vary strongly with its position in the cluster, and a mean radiative
particle cooling term is proposed for single particle simulations of particle
clusters or for high detail simulation, like Direct Numerical Simulations of
small sub-volumes of large clusters of particles. Radiative cooling is shown to
be important both for furnaces for coal gasification and coal combustion.
Broadening the particle size distribution is found to have just a minor effect
on the radiative particle cooling. This is particularly the case for large and
dense particle clusters where there is essentially no effect of size
distribution broadening at all. For smaller and more dilute particle clusters,
the effect of distribution broadening is clear but still not dominant
A simulation of film cooling in the leading edge region of a turbine blade (trench effect on film effectiveness from cylinder in crossflow)
Film cooling is one of the cooling system techniques applied to the turbine blade.
Gas turbine use film cooling technique to protect turbine blade from expose directly
to a hot gas to avoid the blade from defect. The focus of this investigation is to
investigate the effect of embedded three difference depth of trench at cooling holes
geometry to the film cooling effectiveness. Comparisons are made under blowing
ratio 1.0, 1.25, 1.5 and 2.0. Three configuration leading edge with depth Case A
(0.0125D), Case B (0.0350D) and Case C (0.713D) were compared to leading edge
without trench. Result shows that as blowing ratio increased from 1.0 to 1.25, the
film cooling effectiveness is increase for leading edge without trench and also for all
cases. However when the blowing ratio is increase to 1.5, film cooling effectiveness
is decrease for all cases. Meanwhile for blowing ratio 2.0, the result shows the effect
of depth is too small for all the cases. Overall the Case B with blowing ratio 1.25 has
the best film cooling effectiveness with significant improvement compared to leading
edge without trench and with trench Case A and Case C
Atmospheric teleconnection mechanisms of extratropical North Atlantic SST influence on Sahel rainfall
Extratropical North Atlantic cooling has been tied to droughts over the Sahel in both paleoclimate observations and modeling studies. This study, which uses an atmospheric general circulation model (GCM) coupled to a slab ocean model that simulates this connection, explores the hypothesis that the extratropical North Atlantic cooling causes the Sahel droughts via an atmospheric teleconnection mediated by tropospheric cooling. The drying is also produced in a regional climate model simulation of the Sahel when reductions in air temperature (and associated geopotential height and humidity changes) from the GCM simulation are imposed as the lateral boundary conditions. This latter simulation explicitly demonstrates the central role of tropospheric cooling in mediating the atmospheric teleconnection from extratropical North Atlantic cooling. Diagnostic analyses are applied to the GCM simulation to infer teleconnection mechanisms. An analysis of top of atmosphere radiative flux changes diagnosed with a radiative kernel technique shows that extratropical North Atlantic cooling is augmented by a positive low cloud feedback and advected downstream, cooling Europe and North Africa. The cooling over North Africa is further amplified by a reduced greenhouse effect from decreased atmospheric specific humidity. A moisture budget analysis shows that the direct moisture effect and monsoon weakening, both tied to the ambient cooling and resulting circulation changes, and feedbacks by vertical circulation and evaporation augment the rainfall reduction. Cooling over the Tropical North Atlantic in response to the prescribed extratropical cooling also augments the Sahel drying. Taken together, they suggest a thermodynamic pathway for the teleconnection. The teleconnection may also be applicable to understanding the North Atlantic influence on Sahel rainfall over the twentieth century
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