首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Terrestrial photogrammetric techniques applied to the control of a parabolic dune in the Liencres dune system, Cantabria (Spain)
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Terrestrial photogrammetric techniques applied to the control of a parabolic dune in the Liencres dune system, Cantabria (Spain)

机译:地面摄影测量技术,用于控制坎塔布里亚(西班牙)Liencres沙丘系统中的抛物线沙丘

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摘要

The spatial-temporal variations of a dune system can be determined by using diverse 'geomatic' methodologies: geodesy, global positioning system (GPS) and photogrammetry. In the case of the Liencres dune system, a study will be carried out using the 'close-range' photogrammetry technique and the topography technique (total station and GPS). In order to determine the dynamic of the dune system it is necessary to repeat the process of study after a specific interval of time. For this reason, three dimensional data should be available in two different time periods, between which the displacement of the object of analysis (the front portion of the dune) will he significant enough to evaluate its magnitude. This work analyses the viability or photogrammetry For the determination or the spatial-temporal changes of a coastal paraholic dune. Two factors have been analysed: first, the comparison of the photogrammetric results with the results obtained from topographic methods (total station all([ GPS), and second, the quantification of the displacement of the dune system. The analysis of the correspondence between the movement of different parts of the dune and the influence of the intensity and direction of the prevailing wind in the area is also desired. The dune advanced 12-15 +/- 0-06 in (an average of 8.5 m/yr), and the partial implications for the dynamic of human modified processes oil the natural park have been established. Copyright (C) 2008 John Wiley & Sons, Ltd.
机译:沙丘系统的时空变化可以通过使用多种“地理”方法来确定:大地测量,全球定位系统(GPS)和摄影测量。在Liencres沙丘系统的情况下,将使用“近距离”摄影测量技术和地形技术(全站仪和GPS)进行研究。为了确定沙丘系统的动态,必须在特定的时间间隔后重复学习过程。因此,应该在两个不同的时间段中获得三维数据,在这两个时间段之间,分析对象(沙丘的前部)的位移将足以评估其大小。这项工作分析了可行性或摄影测量法,用于确定沿海顺丁沙丘或时空变化。分析了两个因素:首先,将摄影测量结果与通过地形学方法获得的结果进行比较(总站数(GPS),其次,对沙丘系统的位移进行量化。还需要沙丘不同部分的移动以及该区域盛行风的强度和方向的影响,沙丘前进12-15 +/- 0-06英寸(平均8.5 m / yr),并且版权所有(C)2008 John Wiley&Sons,Ltd.。

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