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Historical and computational analysis of the long-term environmental change: Forests in the Shenandoah Valley of Virginia.

机译:长期环境变化的历史和计算分析:弗吉尼亚州谢南多厄山谷的森林。

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摘要

The increase and decrease of forests is a major factor of land cover change. This study of forest change in the Shenandoah Valley builds upon the rich historiography of the region through the analysis of generalized and spatially explicit primary and secondary sources covering the period of 1700 to 2000. Combining geo-historical and geo-computational approaches produced a more robust picture of land cover change than would be possible using only one method. Comparing modern and historical reports on the timing of forest clearance and re-growth revealed that a discrepancy existed between the spatially explicit sources and existing historical interpretations regarding the timing and location of forest clearance and re-growth. Understanding this discrepancy is important for the interpretation of forest change and its implications in the Shenandoah Valley and beyond.; Two main aspects of the study are the thorough interrogation and comparison of different data sources, and the subsequent analysis and interpretation of the data. Historic maps (1864, 1906, and c. 1945) and digital data sets derived from remotely sensed images (c. 1974 and c. 1992) were analyzed in a geographic information system (GIS) and compared to agricultural census data and published reports of land use and land cover change. Three major findings came out of this study. First, the spatially explicit sources produced values for the amount of cleared area that were within 0.5 to 2.7% of the same information derived from the agricultural census. Second, the maximum amount of forest clearance occurred 25--50 years later than existing published reports indicated. Third, the commonly held explanations of federal land acquisition and the abandonment of farms on steep slopes did not account for the observed patterns of forest re-growth. The documented variations in spatial and temporal patterns and reasons for the variations have impacts on our understanding of cultural and physical processes that took place in the region.
机译:森林的增加和减少是土地覆盖变化的主要因素。该雪南多厄河谷森林变化研究基于该地区丰富的历史学,通过分析涵盖1700年至2000年的广义和空间明确的主要和次要来源。结合地理历史和地理计算方法产生了更强大的结果土地覆被变化的图片比仅使用一种方法可能得到的效果要好。比较有关森林砍伐和重新生长的时间的现代和历史报告表明,空间明确的资源与现有的关于森林砍伐和重新生长的时间和位置的历史解释之间存在差异。理解这种差异对于解释森林变化及其在雪兰多厄河谷及以后地区的意义非常重要。研究的两个主要方面是对不同数据源的彻底询问和比较,以及对数据的后续分析和解释。在地理信息系统(GIS)中分析了历史地图(1864、1906和1945年)和从遥感图像(1974年和1992年)获得的数字数据集,并将其与农业普查数据和已发布的报告进行了比较土地利用和土地覆被变化。这项研究得出了三个主要发现。首先,空间明晰的来源所产生的清除面积的值在农业普查得出的相同信息的0.5%至2.7%之内。第二,最大的森林砍伐发生时间比现有已公布的报告晚了25--50年。第三,关于联邦土地征用和在陡坡上放弃农场的普遍解释并不能解释所观察到的森林再生方式。记录在案的时空格局变化以及变化的原因会影响我们对该地区发生的文化和自然过程的理解。

著录项

  • 作者

    Wilson, James William.;

  • 作者单位

    University of Maryland, College Park.;

  • 授予单位 University of Maryland, College Park.;
  • 学科 Physical Geography.; Agriculture Forestry and Wildlife.; Environmental Sciences.
  • 学位 Ph.D.
  • 年度 2005
  • 页码 147 p.
  • 总页数 147
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 自然地理学;森林生物学;环境科学基础理论;
  • 关键词

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