排序方式： 共有7条查询结果，搜索用时 250 毫秒
1
1.
2.
The amount of methane leaked from deep sea cold seeps is enormous and potentially affects the global warming,ocean acidification and global carbon cycle. It is of great significance to study the methane bubble movement and dissolution process in the water column and its output to the atmosphere. Methane bubbles produce strong acoustic impedance in water bodies, and bubble strings released from deep sea cold seeps are called "gas flares"which expressed as flame-like strong backscatter in the water column. We characterized the morphology and movement of methane bubbles released into the water using multibeam water column data at two cold seeps. The result shows that methane at site I reached 920 m water depth without passing through the top of the gas hydrate stability zone(GHSZ, 850 m), while methane bubbles at site II passed through the top of the GHSZ(597 m) and entered the non-GHSZ(above 550 m). By applying two methods on the multibeam data, the bubble rising velocity in the water column at sites I and II were estimated to be 9.6 cm/s and 24 cm/s, respectively. Bubble velocity is positively associated with water depth which is inferred to be resulted from decrease of bubble size during methane ascending in the water. Combined with numerical simulation, we concluded that formation of gas hydrate shells plays an important role in helping methane bubbles entering the upper water bodies, while other factors, including water depth, bubble velocity, initial kinetic energy and bubble size, also influence the bubble residence time in the water and the possibility of methane entering the atmosphere. We estimate that methane gas flux at these two sites is 0.4×10~6–87.6×10~6 mol/a which is extremely small compared to the total amount of methane in the ocean body, however, methane leakage might exert significant impact on the ocean acidification considering the widespread distributed cold seeps. In addition, although methane entering the atmosphere is not observed, further research is still needed to understand its potential impact on increasing methane concentration in the surface seawater and gas-water interface methane exchange rate, which consequently increase the greenhouse effect. 相似文献
3.
4.
5.
6.
多波束测深数据广泛服务于水下地形测量。一些基于测深数据的应用需要提取测深数据的边缘轮廓和探测数据中的空洞。针对已有边缘识别算法执行效率低、边界点提取不完整等问题,通过分析点云模型的局部几何属性,提出一种新的基于k-d树的由粗到精的边缘提取算法。首先抽稀测深数据,基于k-d树建立散乱点云的拓扑关系;然后计算散乱点云法向量,采用距离及角度阈值法进一步提取孔洞与边缘轮廓点并去除错误识别的点;最后基于凹包算法,精确获取边缘轮廓点。在西太平洋海域的实验表明：相较于Alpha-shape和Boundary estimation算法,本算法能够更为精确地识别出散乱点云中的边界点,实用性强。 相似文献
7.
1