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21.
We investigate the influence of low-frequency Rossby waves on the thermal structure of the upper southwestern tropical Indian
Ocean (SWTIO) using Argo profiles, satellite altimetric data, sea surface temperature, wind field data and the theory of linear
vertical normal mode decomposition. Our results show that the SWTIO is generally dominated by the first baroclinic mode motion.
As strong downwelling Rossby waves reach the SWTIO, the contribution of the second baroclinic mode motion in this region can
be increased mainly because of the reduction in the vertical stratification of the upper layer above thermocline, and the
enhancement in the vertical stratification of the lower layer under thermocline also contributes to it. The vertical displacement
of each isothermal is enlarged and the thermal structure of the upper level is modulated, which is indicative of strong vertical
mixing. However, the cold Rossby waves increase the vertical stratification of the upper level, restricting the variability
related to the second baroclinic mode. On the other hand, during decaying phase of warm Rossby waves, Ekman upwelling and
advection processes associated with the surface cyclonic wind circulation can restrain the downwelling processes, carrying
the relatively colder water to the near-surface, which results in an out-of-phase phenomenon between sea surface temperature
anomaly (SSTA) and sea surface height anomaly (SSHA) in the SWTIO. 相似文献
22.
Junqiao Feng Dunxin Hu Fei-fei Jin Fan Jia Qingye Wang Shoude Guan 《Journal of Oceanography》2018,74(5):523-539
The Pacific interior subtropical?tropical cells (STCs) and their relation to the two types of El Niño-Southern Oscillation (ENSO) are investigated by using GODAS reanalysis ocean data for the period of 1980–2017. The results show that the interior STC transport into the equatorial region across 9°S and 9°N has a close relationship with the eastern Pacific (EP) ENSO, while it is much weaker with the central Pacific (CP) ENSO. It is suggested that the effect of interior STCs on the tropical Pacific climate is reflected in its relation with the western Pacific thermocline depth or SSHA. During the EP El Niño, the anomalous interior STCs at 9°S and 9°N converge to the equatorial region from the lag months of ? 25 to ? 8, leading to an accumulation of heat content in the equatorial Pacific; from the lag months of ? 8 to 10, they diverge poleward, inducing a discharge of equatorial heat content. The peak poleward interior STC anomaly first appears at 9°N at a zero-lag time, while that at 9°S is observed 4–5 months later. But there is also no appearance of a time lag between the interior STCs at 9°N and 9°S in recharging the period during the EP La Niña mature phase. However, during CP El Niño, only the conspicuous anomalous interior STC divergence appears during the mature and decay phases for the lag months of ? 2 to 10, with being symmetric at 9°N and 9°S. 相似文献
23.
Automatic conversion of IFC datasets to geometrically and semantically correct CityGML LOD3 buildings 总被引：1，自引：0，他引：1 
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下载免费PDF全文 Although the international standard CityGML has five levels of detail (LODs), the vast majority of available models are the coarse ones (up to LOD2, i.e. block‐shaped buildings with roofs). LOD3 and LOD4 models, which contain architectural details such as balconies, windows and rooms, rarely exist because, unlike coarser LODs, their construction requires several datasets that must be acquired with different technologies, and often extensive manual work is needed. In this article we investigate an alternative to obtaining CityGML LOD3 models: the automatic conversion from already existing architectural models (stored in the IFC format). Existing conversion algorithms mostly focus on the semantic mappings and convert all the geometries, which yields CityGML models having poor usability in practice (spatial analysis, for instance, is not possible). We present a conversion algorithm that accurately applies the correct semantics from IFC models and that constructs valid CityGML LOD3 buildings by performing a series of geometric operations in 3D. We have implemented our algorithm and we demonstrate its effectiveness with several real‐world datasets. We also propose specific improvements to both standards to foster their integration in the future. 相似文献
24.
Long wavelength baroclinic oceanic Rossby waves are of interest because they are the main mechanism of energy transfer among the oceanic basins as the rotating fluid adjusts under the forcing of gravity and buoyancy,They play an important role in dynamics and thermodynamics in the ocean.The signature of them is evident from the altimeter measurements.Sea surface beight derived from the multiple ocean satellite altimeter missions over 1993～2008 is analyzed to systematically investigate the characteristics of the Rossby waves in the tropical Indian Ocean,by jointly adopting 2D-FFT,2D-Radon Transform,Complex Empirical Orthogonal Function and the classic linear theory methods.Results are as follows.The energy of Rossby wave is mainly concentrated between 5°S～18°S.Annual Rossby wave can be observed all over the whole badin,whereas semi-annual Rossby wave can bw only detected in the equatorial area, and inter-annual Rossby wave in the off-equatorial region.The phase speeds of Rossby waves detected from altimeter satellites are basically in agreement with the calculation based on the classic linear theory, but the former are some slower(faster) north(south)of 15°S than the later,Furthemore,it is indicated from the CEOF analysis that the annual Rossby waves is apparent in the Bay of Bengal,Arabian Sea ,and the open south Indian Ocean,whereas inter-annual Rossby wave mainly presents in the south Indian Ocean ,and eastward Kelvin wave is dominant along equator. 相似文献
25.
断层圈闭是斜坡区重要的构造圈闭类型,为了识别斜坡区断层圈闭发育部位及其形成时期,基于断层生长机制,分析斜坡区顺向断层圈闭和反向断层圈闭形成演化过程。结果表明：顺向断层圈闭形成于断层"硬连接"阶段,发育在断层下降盘分段生长部位;反向断层圈闭形成于断层开始活动时期,发育在断层上升盘位移最大部位。在此基础上,充分利用详细三维地震资料,结合断距-距离曲线、相干体切片、断层分段生长时期定量表征以及断距回剥等技术,建立了斜坡区断层圈闭发育部位及形成时期的识别方法,并将该方法应用于冀中坳陷文安斜坡典型断层圈闭发育部位及形成时期的识别,研究结果与实际油气分布吻合关系较好。 相似文献