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1.
?????BP??????????????????Kalman????????????????????????????????????BP???????÷????????BP?????????????????????????????????????????????÷??????????????????????Ч??????  相似文献   

2.
����Bayesian����BP�������GPS�߳�ת��   总被引:2,自引:0,他引:2  
?????BP?????????????????????????????????????Bayesian?????????BP??????????????????????????GPS??????????????????L-M????????????????????????Bayesian??????BP????????????????????????????????????  相似文献   

3.
???BP??????????????С???????????BP?????缤????????BP????????????????????????????????С???????磬??Ч?????????????????????????????????????????????????????????Ч????  相似文献   

4.
?????α????????????????????????????BP???????????????α??????????????????????????????????????????????????????????????????????????????????BP??????????????????Ч????  相似文献   

5.
???????BP???????????????????????????????????????????????????????????????????б?????????????????????Ч???????÷???????????????????????????????????????????緽????????????ж??ó????????????BP???????????????????????????  相似文献   

6.
??????????????BP?????緽??????????ι???????????????????????????????BP????????,???????ж?????????С????????????????С????????,???????????????????????????,?÷??????к??????????????????????  相似文献   

7.
基于BP神经网络的企业效绩综合评价方法   总被引:5,自引:0,他引:5  
为了建立企业效绩综合评价模型,在由基本的财务指标构成的财务分析体系基础上,将BP神经网络应用于效绩综合评价中.以企业历史数据作为BP神经网络的训练样本,用训练好的BP网络评价企业当期各方面的效绩.试验结果表明将BP网络应用于企业评价中,能达到令人满意的评价效果.  相似文献   

8.
???GPS???????????????????????????y?????????BP?????編??????????????????????6????????????????????????????????????6?????????????????????????????BP?????編???????????3????????????????????  相似文献   

9.
???BP???????????????????????????????????????????????????????G??P??????????????????????????????????????D??h?????????????????m????????????????????????????????????????????????????BP????????????????????????????????????????????е??????????????????????????????????????????????????????????????????????t?????????????  相似文献   

10.
This study focuses on sedimentary environmental changes offshore of Hangzhou Bay,East China,since the Late Quaternary. AMS 1 4 C ages from core CJK10,lithologies,distribution of foraminifera,heavy minerals,and S and Cl elements show a f luvial terrace environment during ~23.2–11.0 cal ka BP; a littoral to tidal-f lat environment during 11.0–10.2 cal ka BP; and a shallow marine environment with a relatively low sedimentation rate(0.1–0.22 cm/a) since 4.3 cal ka BP. High depositional rates(~1.6 cm/a) from 10.9 to 10.2 cal ka BP resulted from suff icient accommodation space created by rapid sea level rise from-44 m to-33 m,from high sediment delivery by local rivers,and effective trapping of sediments by tidal-f lat vegetation. The rate of sea level rise was variable; relatively high from 10.9 to 10.6 cal ka BP(2.1 cm/a),and lower since 10.6 cal ka BP(1.2 cm/a). The Changjiang alongshore current crossed the Hangzhou Bay to form the mud wedge on the inner shelf of the East China Sea later than 9.4 cal ka BP. The CJK10 site was a tide-dominated shelf environment and experienced erosion from approximately 9.4–9.2 cal ka BP to 4.3 cal ka BP. The depositional hiatus was caused by the Changjiang alongshore current,which was relatively weak during 9.4–7.5 cal ka BP and increased in strength during ~7.5–4 cal ka BP. From ~4.3 cal ka BP,a large amount of sediment from the Changjiang River was partly deposited on the continental shelf of Hangzhou Bay with some transported southward. Therefore,this study clarif ies the history of Changjiang-derived sediment dispersal and deposition,although a detailed record of the changes in the Changjiang alongshore current since 4.3 cal ka BP is diff icult to obtain because of the scarcity of evidence.  相似文献   

11.
Lake Lop Nur is located in the eastern part of the Tarim Basin in Xinjiang,northwestern China.A 220-cm-long sediment core was collected from the center of the ear-shaped depression forming the basin and dated with AMS~(14)C.Grain size,total organic matter(TOC),total nitrogen(TN),and TOC/TN(C/N)analyses were used to reconstruct climatic conditions from 13.0 to 5.6 cal ka BP.The results showed fi ve main climatic stages.Zone I(13.0–11.3 cal ka BP)was a wet–dry environment,whereas Zone II(11.3–8.9 cal ka BP)consisted of a primarily wet environment.Zone III(8.9–7.7 cal ka BP)was subdivided into Zone IIIa(8.9–8.2 cal ka BP)that indicated lake constriction and dry climate,and Zone IIIb(8.2–7.7 cal ka BP)in which the proxies indicated wet conditions.In Zone IV(7.7–6.6 cal ka BP),the climate presented a bit wet conditions.In Zone V(6.6–5.6 cal ka BP),abundant glauberite is present in the sediment and silt dominates the lithology;these results indicate the lake shrank and the overall climate was dry.Abrupt environmental events were also identifi ed,including six dry events at 11.0,10.5,9.3,8.6,8.2,and 7.6 cal ka BP and one fl ood event from 7.8 to 7.7 cal ka BP in the Early–Middle Holocene.  相似文献   

12.
BP网络分类方法是一种新的模式识别方法,在遥感图像分类识别处理中有良好的应用前景。文章在阐明BP网络组成的基础上,介绍了BP网络的遥感图像分类过程,指出应注意的一些问题,并分析了其应用效果。  相似文献   

13.
采取混沌映射和自适应惯性权重结合的策略对标准鲸鱼算法进行改进,从而提高算法的全局寻优能力和收敛速度,并针对BP神经网络的劣势,利用改进鲸鱼算法对BP神经网络进行优化处理。在此基础上建立改进鲸鱼算法优化BP神经网络的GPS高程异常拟合预测模型,并通过两组不同地形特征工程中的GPS数据对模型进行验证。结果表明,利用改进鲸鱼算法优化的BP模型进行GPS高程拟合时可取得更高的精度和稳定性。  相似文献   

14.
BP神经网络、GA-BP神经网络及SVR模型是机器学习领域常用的三种预测方法,但在登革热预测方面鲜有人涉及。本文以广州市主城区登革热预测为例,对比BP神经网络、GA-BP神经网络及SVR模型在登革热时空预测上的作用,比较三种模型在登革热时空动态预测中的优劣性。研究表明,1从模型预测效果上看,SVR模型稳定,预测效果显著优于BP及GA-BP模型;2从模型性能上看,GA-BP模型优于BP及SVR模型; 3SVR与GA-BP模型在登革热预测上切实可行。  相似文献   

15.
为了发现电子政务内网的信息安全隐患,提出一种将层次分析法(AHP)与反向传播人工神经网络(BP ANN)技术相结合的内网信息安全评估方法,基于AHP与BP ANN分别建立模型共同完成评估。以电子政务内网信息安全指标作为样本,利用AHP模型得到指标体系第二层的指标值,再以AHP模型输出值为样本对BP ANN评估模型进行学习和训练,找到输入与输出之间的关系,并对训练好的BP网络进行验证。仿真结果表明,评估方法能够为复杂的电子政务内网进行信息安全评估,评估模型稳定且自适应性强。  相似文献   

16.
针对传统BP神经网络存在的学习速度慢、易陷入局部极值等问题,利用鲸鱼优化算法(WOA)以及狼群算法(WPA)混合优化BP神经网络的权值和阈值,构建WPA-WOA-BP神经网络模型,并对PM2.5浓度进行预测。实验结果证明,WPA-WOA-BP神经网络模型预测稳定性高,可用于PM2.5浓度的预测,且预测精度优于BP神经网络、WPA-BP神经网络和WOA-BP神经网络模型。  相似文献   

17.
在区域地质构造调查、地球物理资料和遥感解译基础上,采用钻探、槽探、14C年代学测试等方法,对伊通-舒兰断裂带四平段NE向隐伏断层的时代、性质及构造意义进行探讨。结果表明:1)四平段断裂主要发育于上更新统长英质(含角砾)砂岩层内部,为逆冲推覆断层;2)槽探与钻孔揭露的耕土层、粘土层、泥质砂岩层和长英质(含角砾)砂岩层AMS14C测年结果分别为-70~6 270 BP、60~7 780 BP、110~21 780 BP和11 740~26 100 BP,断层活动年代总体应归属为前第四纪(>26 100 BP);3)结合区域岩浆构造与地震事件可知,本次揭露的NE向隐伏断裂带可能形成于晚更新世。  相似文献   

18.
通过对藏北高原西北部结则茶卡湖泊及其沿岸地质地貌调查,发现其为一个富含硼、锂、钾、锶的封闭型盐湖,沿岸海拔4 850 m拔湖325 m有一条明显的高位湖岸线,该湖岸线到湖面之间有六级湖积阶地发育,六级以上阶地保存零星。沿湖岸不同高度上的湖积物U系年龄分别为(14.2±1.2)ka BP(T2)、(38.0±3.5)ka BP(T4)和(41.6±3.2)ka BP(T5)。湖面下降的幅度是藏北高原迄今所知最大。根据湖面平均下降速度推算高位湖岸线和高位湖积层的形成年龄在(120~90)ka BP,与东部的纳木错和西部的甜水海基本一致,说明藏北高原在晚更新世初期有一个明显的泛湖期。大约100 ka BP结则茶卡湖面开始下降,晚更新世以来湖泊演化是在封闭体系干旱环境下进行的,盐湖形成于14 ka BP左右,藏北高原在晚更新世以来气候变化可能为自西向东逐渐变为干寒。  相似文献   

19.
根据2003-2011年渔汛期间我国鱿钓船在西南大西洋海域的生产统计数据,结合海洋遥感获得的海表温度(SST)和海面高度(SSH)等数据,以单位捕捞努力量渔获量(CPUE)和作业次数作为中心渔场指标,以月份、经度、纬度、SST和SSH为输入因子,利用BP神经网络方法构建西南大西洋阿根廷滑柔鱼中心渔场预报模型。比较14种不同结构的BP神经网络模型,以CPUE作为中心渔场预报指标的BP模型均较佳,其拟合残差范围为0.004 0~0.005 5,平均值为0.004 7;而以作业次数作为中心渔场预报指标的BP模型,其拟合残差范围为0.009 3~0.011 6,平均值为0.010 4。输入因子为月份、经度、纬度、SST和SSH,输出因子为初值化后的CPUE,网络结构为5-4-1时的BP神经网络模型为最佳,其拟合残差为0.004 025,该模型可用于阿根廷滑柔鱼中心渔场的预报。BP神经网络方法可为准确渔场预报提供新途径。  相似文献   

20.
在简要分析BP算法的基础上 ,应用BP网络的理论与方法 ,选取地下水位、临界深度、平均标准贯入击数、地面最大加速度、震动持续时间作为指标 ,评价砂土震动液化 ,取得了较好的评价效果。  相似文献   

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