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Assessing the seasonal dynamics of inundation, turbidity, and aquatic vegetation in the Australian wet–dry tropics using optical remote sensing

机译:利用光学遥感评估澳大利亚湿热带地区淹没,浑浊和水生植被的季节动态

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摘要

Floodplain wetlands in the wet-dry tropics are under increasing pressure from water resource development, and there is a need for methods to assess the biophysical dynamics of these extensive and often remote ecosystems. This study assessed the capacity of optical remote sensing methods to monitor the seasonal dynamics of inundation, turbidity, and aquatic vegetation cover for a northern Australian savanna catchment. MODIS data were used to map seasonal flood inundation patterns, and Landsat 5 TM data were used to map dry-season waterbody dynamics. A network of water-depth loggers and temperature sensors provided ground observations of surface inundation dynamics, and was used to validate the inundation mapping. Post-flood waterbody surface area declined by 89% over the dry season, with 70% of the decline occurring for Palustrine (floodplain) waterbodies. All aquatic systems became increasingly disconnected as the dry season progressed. Statistical relationships were developed between seasonal measurements of turbidity, aquatic vegetation cover, and Landsat spectral data. Catchment wide predictions showed that turbidity increased and macrophyte cover decreased for the Palustrine and Lacustrine (lake) systems, while the Riverine systems became less turbid over the dry season. These results show that, for open savanna landscapes where cloud cover does not limit waterbody detection, optical remote sensing methods can be effectively applied to assess seasonal patterns of inundation and accompanying biophysical dynamics. This provides an effective tool to evaluate the impact of river flow regime changes from water resource use or climate change in these regions.
机译:湿干热带地区的洪泛区湿地正面临着水资源开发带来的越来越大的压力,因此需要一种方法来评估这些广泛且通常是偏远的生态系统的生物物理动态。这项研究评估了光学遥感方法监测北澳大利亚大草原流域的淹没,浑浊和水生植被覆盖季节动态的能力。 MODIS数据用于绘制季节性洪水淹没模式,Landsat 5 TM数据用于绘制旱季水体动态。水深记录仪和温度传感器网络可提供地面对表面淹没动力学的观测,并用于验证淹没图。洪灾后的水体表面积在干旱季节下降了89%,其中70%的下降发生在Palustrine(洪泛平原)水体上。随着旱季的进行,所有水生系统的联系日益疏远。在浊度,水生植被覆盖度和Landsat光谱数据的季节性测量之间建立了统计关系。流域范围内的预测表明,Palustrine和Lacustrine(湖)系统的浊度增加而大型植物的覆盖率降低,而Riverine系统在旱季变得较不浑浊。这些结果表明,对于开阔的热带稀树草原景观而言,云量并不限制水体的探测,光学遥感方法可以有效地用于评估淹没的季节性模式及其伴随的生物物理动力学。这为评估这些地区水资源利用或气候变化对河流水流变化的影响提供了有效的工具。

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