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481.
Turbulent measurements in the stable atmospheric boundary layer during SHEBA: ten years after 总被引:4,自引:0,他引:4
Andrey A. Grachev Edgar L. Andreas Christopher W. Fairall Peter S. Guest P. Ola G. Persson 《Acta Geophysica》2008,56(1):142-166
This paper surveys results of the comprehensive turbulent measurements in the stable boundary layer (SBL) made over the Arctic
pack ice during the Surface Heat Budget of the Arctic Ocean experiment (SHEBA) in the Beaufort Gyre from October 1997 through
September 1998. Turbulent fluxes and mean meteorological data were continuously measured and reported hourly at five levels
on a 20-m main SHEBA tower. Eleven months of measurements during SHEBA cover a wide range of stability conditions, from the
weakly unstable regime to very stable stratification, and allow studying the SBL in detail.
A brief overview of the SBL regimes, the flux-profile relationships, the turbulent Prandtl number, and other parameters obtained
during SHEBA is given. The traditional Monin—Obukhov approach, z-less scaling, and gradient-based scaling are evaluated and discussed based on the data from SHEBA. 相似文献
482.
Vesiculation and crystallization in ascending magmas are key processes that control the eruption behavior, and they interplay each other through the water exsolution process. We conducted a numerical study in order to quantitatively understand the water exsolution and crystallization processes in natural eruptions (decompression history is unknown) and in laboratory experiments (the amount of decompression is constant with time). The numerical results, which take into account homogeneous or heterogeneous nucleation and growth of bubbles with varying diffusivity of water, viscosity, and the amount of decompression, provide a quantitative understanding of their control on bubble formation and water exsolution in the constant amount of decompression. The bubble nucleation in the homogeneous nucleation can be divided into two regimes – the diffusion control regime and viscosity control regime – depending on the modified Peclet number and the effective supersaturation. In the cases of both homogeneous and heterogeneous nucleations, the bubble growth is controlled by diffusion or viscosity, depending on the modified Peclet number and bubble number density. The water exsolution rate, which is controlled by the modified Peclet number in the viscosity control regime and by the bubble number density and diffusive driving force in the diffusion control regime, acts as an effective cooling rate in a decompression-induced crystallization process. A comparison of the numerical results with the results of laboratory experiments suggests that water exsolution proceeds by the diffusion-limited growth of bubbles under disequilibrium vesiculation through the heterogeneous nucleation of bubbles, and this in turn controls the crystallization kinetics of microlite with the homogeneous nucleation of microlite and the diffusion-limited growth of crystal. The several orders of variation of microlite number density with the amount of decompression in laboratory experiments can be interpreted as the effect of the amount of decompression on the driving force for the diffusive bubble growth that controls the water exsolution rate. 相似文献
483.
足尺钢框架振动台试验及动力弹塑性数值模拟 总被引:4,自引:1,他引:3
本文通过有限元分析程序OpenSees对一足尺四层钢框架结构进行静力及动力弹塑性分析,结构构件采用自由度较少的纤维模型模拟。在振动台试验之前,预测足尺钢框架结构连续在小震、中震及大震作用下的响应,将预测分析结果与振动台试验结果进行对比,结果显示该数值模拟方法能很好地反映结构的弹塑性行为及破坏机制,准确预测结构的地震响应及大震下结构倒塌时间。这进一步说明基于纤维模型的整体结构弹塑性分析方法,由于自由度数少,适用于整体结构抗震分析。 相似文献
484.
陈培善 《地震学报(英文版)》2008,21(6):670-671
Illustration All the data in this catalog are chosen from the "Preliminary Seismological Report of Chinese Seismic Stations" (Its abbreviation is "Monthly Report").The catalog includes the events of 相似文献
485.
陈培善 《地震学报(英文版)》2008,21(5):548-552
Illustration All the data in this catalog are chosen from the "Preliminary Seismological Report of Chinese Seismic Stations" (Its abbreviation is "Monthly Report").The catalog includes the events of 相似文献
486.
487.
JAN Chyan-Deng 《中国海洋工程》1998,(4)
—When a 2-D progressive wave train normally or obliquely approaches a vertical wall and thenis normally or obliquely reflected from it,the combination of the approaching and reflected waves may re-sult in a standing wave or a short-crested wave in front of the wall.This paper presents the experimentalobservations of sand bed configurations under the action of these water waves in front of the wall.The ge-ometry of sand ripples under these water waves in front of the vertical wall is presented as a function offlow parameters,such as the water particle semi-excursion and the mobility number. 相似文献
488.
489.
单视数SAR图像Speckle滤波方法的研究 总被引:2,自引:0,他引:2
在分析单机数SAR影像的Speckle局部统计特性和现有的空间滤波算法的基础上,提出了一种新的Speckle滤波方法,该方法采用特殊的滤波窗口邻域划分方法,根据窗口相对标准差自适应地调整窗口尺寸和窗口内的滤波区域。该方法被用于多幅单视数ERS-1/2SAR图像去Speckle处理,并与以往的典型算法进行了比较,取得了较好的实验结果。 相似文献
490.
相关观测情况的可靠性研究 总被引:12,自引:3,他引:9
可靠性是测量网优化设计和数据质量控制要考虑的重要因素之一。在独立观测情况,测量网的可靠性可用多余度(或称多余观测分量)来表示,多余度越小,该余度越小,该观测位置的可靠性越差,但在相关观测情况,多余度的值域超出(0,1)区间,已不能可靠性特征。本文建议采用一种新的可靠性度量指标:ri=(PR)ii/Pii,其中P是观测权阵,R是平差因子阵。ri的值域在一种新的可靠性度量指标;ri=(PR)ii/pi 相似文献