保存洪水扰动的地貌数据记录

GeoResJ Pub Date : 2015-06-01 DOI:10.1016/j.grj.2015.02.016
John A. Moody , Deborah A. Martin , Robert H. Meade
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引用次数: 0

摘要

美国目前没有中央数据库或存储库来保存长期的、空间上广泛的河流地貌数据记录,或提供未来的可访问性。然而,由于它们的长度和连续性,这些数据对未来的研究是有价值的。因此,我们建立了一个公众可访问的网站,以保存两个长期监测实例(40年和18年)对自然干扰的河流地貌响应的数据记录。第一次扰动是1978年蒙大拿州粉河发生的50年一遇的洪水,第二次扰动是1996年科罗拉多州山火后发生的100年一遇的暴雨后发生的春溪特大洪水。关于保存河流地貌数据,出现了两个关键问题。第一个是保存数据本身,第二个也是同样重要的,是保存收集数据的实地研究地点的位置信息,以便将来重新定位和重新调查这些地点。后者允许将长期数据集扩展到未来,并为解释未来景观变化提供关键的背景数据。数据保存在一个网站上,以便全世界都能访问,并在新数据可用时将其上传到该网站。我们描述了网站的架构,在开发网站的经验教训,未来的改进,以及如何保存有关实地研究站点位置的信息的建议。
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Preserving geomorphic data records of flood disturbances

No central database or repository is currently available in the USA to preserve long-term, spatially extensive records of fluvial geomorphic data or to provide future accessibility. Yet, because of their length and continuity these data are valuable for future research. Therefore, we built a public accessible website to preserve data records of two examples of long-term monitoring (40 and 18 years) of the fluvial geomorphic response to natural disturbances. One disturbance was ∼50-year flood on Powder River in Montana in 1978, and the second disturbance was a catastrophic flood on Spring Creek following a ∼100-year rainstorm after a wildfire in Colorado in 1996.

Two critical issues arise relative to preserving fluvial geomorphic data. The first is preserving the data themselves, but the second, and just as important, is preserving information about the location of the field research sites where the data were collected so the sites can be re-located and re-surveyed in the future. The latter allows long-term datasets to be extended into the future and to provide critical background data for interpreting future landscape changes. Data were preserved on a website to allow world-wide accessibility and to upload new data to the website as they become available. We describe the architecture of the website, lessons learned in developing the website, future improvements, and recommendations on how also to preserve information about the location of field research sites.

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