“海上虚拟人口”假说及其应用探索          下载免费PDF全文

刘大海  安晨星  李森  纪瑞雪 《海洋开发与管理》2018,35(12):3-7

为解决海洋社会经济数据难以获取的问题,促进海洋空间评价的科学化和标准化,文章提出"海上虚拟人口"假说,并对其应用进行探索。研究结果表明:"海上虚拟人口"不是海上实际常住人口,而是对陆上人口数据进行插值后所形成的虚拟人口分布;某一海域的虚拟人口一般按照该海域与海岸线的距离进行插值,距海岸线近的数量多,距海岸线远的数量少;"海上虚拟人口"是海洋社会经济数据的载体之一,其数量可间接反映海洋开发利用水平和海洋社会经济状况;应用步骤包括确定海岸线形状、划分网格单元、修正原始数据和插值计算4个部分。目前"海上虚拟人口"假说及其应用仍处于探索阶段,需在实践中不断检验和完善。  相似文献   

海南岛西海岸沙丘形成动力过程的风洞模拟试验   总被引：3，自引：0，他引：3  

李森  刘贤万  李会川  郑影华  魏兴琥 《地理学报(英文版)》2007,17(4):453-468

The western coast of Hainan Island exhibits a savanna landscape. Many types of sand dunes, including transverse dune ridges, longitudinal dune ridges, elliptical dunes, coppice dunes, and climbing dunes, are widely distributed in the coastal zone. In winter, high-frequency and high-energy NE winds (dominant winds) are prevalent, with a resultant drift direction (RDD) of S35.6°W. In spring, low-frequency and low-energy SW secondary winds prevail, with a RDD of N25.1°E. Wind tunnel simulations revealed that the airflow over the dune surface is the main factor controlling the erosion and deposition patterns of dune surfaces and the morphological development of dunes. In the region’s bidirectional wind en- vironment, with two seasonally distinct energy levels, the airflow over the surface of elliptical dunes, barchan dunes, and transverse dune ridges will exhibit a transverse pattern, whereas the airflow over longitudinal dunes ridges exhibits a lateral pattern and that over climbing dunes exhibits a climbing-circumfluent pattern. These patterns represent different dynamic processes. The coastal dunes on the western coast of Hainan Island are influenced by factors such as onshore winds, sand sources, coastal slopes, rivers, and forest shelter belts. The source of the sand that supplements these dunes particularly influences the development pattern: when there is more sand, the pattern shows positive equilibrium deposition between dune ridges and dunes; otherwise, it shows negative equilibrium deposition. The presence or absence of forest shelter belts also influences deposition and dune development patterns and transformation of dune forms. Coastal dunes and inland desert dunes experience similar dynamic processes, but the former have more diversified shapes and more complex formation mechanisms.  相似文献