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    DsJ+(2632)D_{sJ}^+(2632): An Excellent Candidate of Tetraquarks

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    We analyze various possible interpretations of the narrow state DsJ(2632)D_{sJ}(2632) which lies 100 MeV above threshold. This interesting state decays mainly into DsηD_s \eta instead of D0K+D^0 K^+. If this relative branching ratio is further confirmed by other experimental groups, we point out that the identification of DsJ(2632)D_{sJ}(2632) either as a csˉc\bar s state or more generally as a 3ˉ{\bf {\bar 3}} state in the SU(3)FSU(3)_F representation is probably problematic. Instead, such an anomalous decay pattern strongly indicates DsJ(2632)D_{sJ}(2632) is a four quark state in the SU(3)FSU(3)_F 15{\bf 15} representation with the quark content 122(dsdˉ+sddˉ+suuˉ+usuˉ2sssˉ)cˉ{1\over 2\sqrt{2}} (ds\bar{d}+sd\bar{d}+su\bar{u}+us\bar{u}-2ss\bar{s})\bar{c}. We discuss its partners in the same multiplet, and the similar four-quark states composed of a bottom quark BsJ0(5832)B_{sJ}^0(5832). Experimental searches of other members especially those exotic ones are strongly called for

    Time Delay Compensation and Stability Analysis of Networked Predictive Control Systems Based on Hammerstein Model

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    A novel approach is proposed for a networked control system with random delays containing a nonlinear process based on a Hammerstein model. The method uses a time delay two step generalized predictive control (TDTSGPC), which consists of two parts, one is to deal with the input nonlinearity of the Hammerstein model and the other is to compensate the network induced delays in the networked control system. Theoretical results using the Popov theorem are presented for the closed-loop stability of the system in the case of a constant delay. Simulation examples illustrating the validity of the approach are presented

    Climatic control on the peak discharge of glacier outburst floods

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    Lakes impounded by natural ice dams occur in many glacier regions. Their sudden emptying along subglacial paths can unleash similar to 1 km(3) of floodwater, but predicting the peak discharge of these subglacial outburst floods ('jokulhlaups') is notoriously difficult. To study how environmental factors control jokulhlaup magnitude, we use thermo- mechanical modelling to interpret a 40- year flood record from Merzbacher Lake in the Tian Shan. We show that the mean air temperature during each flood modulates its peak discharge, by influencing both the rate of meltwater input to the lake as it drains, and the lake- water temperature. The flood devastation potential thus depends sensitively on weather, and this dependence explains how regional climatic warming drives the rising trend of peak discharges in our dataset. For other subaerial ice- dammed lakes worldwide, regional warming will also promote higher- impact jokulhlaups by raising the likelihood of warm weather during their occurrence, unless other factors reduce lake volumes at flood initiation to outweigh this effect

    Recent advances on filtering and control for nonlinear stochastic complex systems with incomplete information: A survey

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    This Article is provided by the Brunel Open Access Publishing Fund - Copyright @ 2012 Hindawi PublishingSome recent advances on the filtering and control problems for nonlinear stochastic complex systems with incomplete information are surveyed. The incomplete information under consideration mainly includes missing measurements, randomly varying sensor delays, signal quantization, sensor saturations, and signal sampling. With such incomplete information, the developments on various filtering and control issues are reviewed in great detail. In particular, the addressed nonlinear stochastic complex systems are so comprehensive that they include conventional nonlinear stochastic systems, different kinds of complex networks, and a large class of sensor networks. The corresponding filtering and control technologies for such nonlinear stochastic complex systems are then discussed. Subsequently, some latest results on the filtering and control problems for the complex systems with incomplete information are given. Finally, conclusions are drawn and several possible future research directions are pointed out.This work was supported in part by the National Natural Science Foundation of China under Grant nos. 61134009, 61104125, 61028008, 61174136, 60974030, and 61074129, the Qing Lan Project of Jiangsu Province of China, the Project sponsored by SRF for ROCS of SEM of China, the Engineering and Physical Sciences Research Council EPSRC of the UK under Grant GR/S27658/01, the Royal Society of the UK, and the Alexander von Humboldt Foundation of Germany
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