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Hydrologic responses to climate, water use, land surface transformation, and surface water impoundment in an irrigation intensive watershed.

机译:在灌溉密集的流域中,对气候,用水,土地表层转化和地表蓄水的水文响应。

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摘要

Climatic variability and land surface change have a wide range of often difficult to parse out effects on streamflow. We analyzed long-term records of climate, land use and land cover, and re-constructed the water budget based on precipitation, groundwater levels and water use for the time period from 1950 through 2010 for an irrigation intensive agricultural watershed in the Southern Great Plains, USA.;Increase of surface impounding structures is a unique feature in land surface transformation for the Southern Great Plains. In the United States the highest density of farm ponds is in the Southern Great Plains and specifically in the state of Oklahoma. These represent a significant form of anthropogenic alteration to the landscape. Despite the vast proliferation of these small reservoirs in the state, very few studies have evaluated the ecosystem services and the effects of these water bodies on the hydrologic cycle. We quantified surface water storage in Oklahoma using remote sensing techniques. We qualitatively assess the potential effects of small reservoirs such as farm ponds, stock ponds, animal and industrial waste lagoons, and small flood control reservoirs on streamflow.;For the study period, we found a general trend of increases in grass and woody cover, rapid increase in urban area and surface impoundment. The atmosphere demand (ET0) has trended downward due largely to increase in relative humidity and no trend in temperature change. We found that streamflow was most sensitive to changes in precipitation when annual water consumption for irrigation was high between 1965 and 1984 and was less responsive to precipitation variability since 1985. The changes in the total area of agricultural land and the encroachment of woody species into grassland have been negatively correlated with streamflow over the past 30 years when groundwater pumping has been relatively constant. We found a strong linear correlation between the logs of reservoir capacity and water surface area at multiple spatial scales - state, watershed and county, suggesting a potential in rapid assessment of surface water storage in impounding structures using remote sensing data for this region.;For a watershed with heavy anthropogenic alteration, there is a need to consider drivers aside from the traditional climatic ones and thus, water use, land use and land cover change can all be included in a holistic adaptation and mitigation strategy.
机译:气候变化和土地表面变化通常具有很大的范围,通常很难解析对径流的影响。我们分析了气候,土地利用和土地覆盖的长期记录,并根据1950年至2010年这段时期的降水,地下水位和用水量,重新构造了大平原南部农业密集型农业流域的用水预算美国;;增加表面蓄水结构是南部大平原地区陆地表面转换的独特特征。在美国,最大的池塘密度是在大平原南部,尤其是在俄克拉荷马州。这些代表着人为改变景观的一种重要形式。尽管该州这些小型水库大量扩散,但很少有研究评估生态系统服务以及这些水体对水文循环的影响。我们使用遥感技术对俄克拉荷马州的地表水储量进行了量化。我们定性评估了小型水库(如农场池塘,畜禽池塘,动物和工业废水泻湖以及小型防洪库)对水流的潜在影响;在研究期间,我们发现了草木覆盖率总体呈上升趋势,市区和地表蓄水量迅速增加。大气需求量(ET0)呈下降趋势,这在很大程度上是由于相对湿度的增加而温度没有变化的趋势。我们发现,1965年至1984年之间每年的灌溉用水量很高时,水流对降水变化最敏感,并且自1985年以来对降水变化的响应较小。农业用地总面积的变化和木本植物对草地的侵蚀在过去30年中,当地下水泵送相对稳定时,水流量与流量呈负相关。我们发现在多个空间尺度(州,流域和县)的水库容量和水表面积的测井曲线之间有很强的线性相关性,这表明使用该区域的遥感数据可以快速评估蓄积结构中地表水的储量。在人为改变严重的分水岭上,除了传统的气候因素外,还需要考虑驱动因素,因此,水资源利用,土地利用和土地覆被变化都可以纳入整体的适应和减缓战略中。

著录项

  • 作者

    Dale, Joseph J.;

  • 作者单位

    Oklahoma State University.;

  • 授予单位 Oklahoma State University.;
  • 学科 Hydrology.;Climate Change.;Natural Resource Management.;Water Resource Management.
  • 学位 M.S.
  • 年度 2014
  • 页码 68 p.
  • 总页数 68
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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