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Dynamical Model of a Controlled Parawing for Drop Tests Trajectory Reconstruction

机译：跌落试验轨迹重建控制分布的动态模型

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Bettanini C; Bartolomei M; Aboudan A; Colombatti G;
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2. Neural network and computational fluid dynamics modeling for the gelatinization kinetics of instant controlled pressure drop treated parboiled rice [J] . Chakraborty Sourav, Gautam Swapnil Prashant, Bordoloi Tridisha, Journal of food process engineering . 2020,第11期

机译：肠道控制压力下降凝胶化动力学的神经网络与计算流体动力学建模处理储存稻米
3. Adaptive course control based on trajectory linearization control for unmanned surface vehicle with unmodeled dynamics and input saturation [J] . Mu Dongdong, Wang Guofeng, Fan Yunsheng, Neurocomputing . 2019,第FEBa22期

机译：基于轨迹线性化控制的无模型动力学和输入饱和的无人地面车辆自适应航向控制
4. Reconstruction of stochastic nonlinear dynamical models from trajectory measurements [C] . D.G. Luchinsky, V.N. Smelyanskiy, M. Millonas, Noise in Complex Systems and Stochastic Dynamics III . 2005

机译：基于轨迹测量的随机非线性动力学模型的重构
5. Biome-scale vegetation dynamics in North America since the last glacial maximum: Maps and reconstructions from fossil pollen data and the testing of biogeography models. [D] . Williams, John Warren. 2000

机译：自上次冰川最大期以来北美的生物群落尺度的植被动态：化石花粉数据的地图和重建以及生物地理模型的测试。
6. A Composite Model of Glucagon–Glucose Dynamics for In Silico Testing of Bihormonal Glucose Controllers [O] . Pau Herrero, Pantelis Georgiou, Nick Oliver, 2013

机译：用于双激素葡萄糖控制器计算机模拟测试的胰高血糖素-葡萄糖动力学复合模型。
7. The oceans mediate the response of global climate to natural and anthropogenic forcings. Yet for the past 2,000 years — a key interval for understanding the present and future climate response to these forcings — global sea surface temperature changes and the underlying driving mechanisms are poorly constrained. Here we present a global synthesis of sea surface temperatures for the Common Era (ce) derived from 57 individual marine reconstructions that meet strict quality control criteria. We observe a cooling trend from 1 to 1800 ce that is robust against explicit tests for potential biases in the reconstructions. Between 801 and 1800 ce, the surface cooling trend is qualitatively consistent with an independent synthesis of terrestrial temperature reconstructions, and with a sea surface temperature composite derived from an ensemble of climate model simulations using best estimates of past external radiative forcings. Climate simulations using single and cumulative forcings suggest that the ocean surface cooling trend from 801 to 1800 ce is not primarily a response to orbital forcing but arises from a high frequency of explosive volcanism. Our results show that repeated clusters of volcanic eruptions can induce a net negative radiative forcing that results in a centennial and global scale cooling trend via a decline in mixed-layer oceanic heat content. [O] . McGregor, Helen V., Evans, Michael N., Goosse, Hugues, 2015

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8. FREE-FLIGHT INVESTIGATION OF THE DEPLOYMENT, DYNAMIC STABILITY, AND CONTROL CHARACTERISTICS OF A 1/12-SCALE DYNAMIC RADIO-CONTROLLED MODEL OF A MLARGE BOOSTER AND PARAWING [R] . Sanger M. Burk 1963

机译：自由飞行调查大型推进器和巡航的1/12比例动态无线电控制模型的部署，动态稳定性和控制特性

Dynamical Model of a Controlled Parawing for Drop Tests Trajectory Reconstruction

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