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首页> 外文期刊>Global change biology >Tracking palustrine water seasonal and annual variability in agricultural wetland landscapes using Landsat from 1997 to 2005
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Tracking palustrine water seasonal and annual variability in agricultural wetland landscapes using Landsat from 1997 to 2005

机译:使用Landsat追踪1997年至2005年农业湿地景观中的巴勒斯坦水的季节性和年度变化

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Wetlands densely populate the ecoregion transecting the center of the Prairie Pothole Region (PPR) known as the Missouri Coteau and epicenter to the most productive waterfowl-breeding habitat in North America. These palustrine, depressional basin waters vacillate with regional drought and deluge, so surface water fluctuations over time modulate wetland productivity, habitat, and water quality functions. Models predict formidable effects of climate change on glacial basin surface waters, yet large-scale, long-term observation data are lacking to compare against predicted changes. Current, optical-based water detection models do not delineate marsh vegetation from shallow, turbid, high-chlorophyll waters common to the region. We developed a palustrine wetland spectral model for tracking open surface waters using Landsat imagery, which we evaluated for a 2500 km(2) landscape that estimates seasonal and annual open water variability for thousands of individual wetlands in the Missouri Coteau ecoregion. Detection accuracy of 96% was achieved for water bodies greater than a half-pixel in size. We identified shifts in the distribution of water permanence classes within and between years for waters emerging in spring, mid-summer, and late summer from 1997 to 2005 and identified a maximum of 19 047 basins with open water (12% of the landscape) populating 2500 km(2). For the 2005 growing season, we observed only 8757 basins with open water (6% of the landscape) for the same area. Declines were greatest for water bodies detected only in spring, suggesting a loss of those wetlands functioning to recharge groundwater stores early in the season and a high sensitivity to observed reductions in snowfall. If landscape factors driving open water coverage and wetland density are similar for the entire Missouri Coteau, we estimate the number of basins containing at least a pixel of water for this region declined from 577 600 to 266 000 between 1997 and 2005.
机译:湿地密集于整个生态区,横穿草原坑洼地区(PPR)的中心,被称为密苏里州Coteau,而震中则是北美生产力最高的水禽繁殖栖息地。这些河谷,depression陷盆地水会随区域干旱和洪水而波动,因此地表水随时间的波动会调节湿地的生产力,生境和水质功能。模型可以预测气候变化对冰川盆地地表水的强大影响,但是尚缺乏大规模的长期观测数据来与预测的变化进行比较。当前,基于光学的水探测模型不能从该地区常见的浅,浑浊,高叶绿素水中划定沼泽植被。我们使用Landsat影像开发了一个巴勒斯坦湿地光谱模型,用于跟踪开放的地表水,我们对2500 km(2)的景观进行了评估,该模型估算了密苏里州Coteau生态区数千个湿地的季节性和年度开放水域变化。对于尺寸大于半个像素的水体,检测精度达到96%。我们确定了1997年至2005年春季,夏季和夏季末期间出现的水在多年内和多年之间的水持久性分布的变化,并确定了最多19 047个流域(占景观的12%)流域2500公里(2)。在2005年的生长季节中,我们只观察到8757个同一地区的开阔水域(占景观的6%)。对于仅在春季发现的水体,下降幅度最大,这表明该季节初期失去了补充地下水存储功能的湿地的损失,并且对观测到的降雪量高度敏感。如果整个密苏里州Coteau的景观因素导致开放水域覆盖和湿地密度相似,那么我们估计该地区至少包含一个像素水域的盆地数量在1997年至2005年之间从577 600下降到266 000。

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