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The impact of fire on sand dune stability: Surface coverage and biomass recovery after fires on Western Australian coastal dune systems from 1988 to 2016

机译:火灾对沙丘稳定性的影响:1988年至2016年大火对西澳大利亚州沿海沙丘系统的覆盖和生物量回收

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This study aims to determine the common response of coastal sand dunes in Western Australia (WA) to fire on decadal time-scales, in terms of ecological-geomorphic-climatic interactions to test the hypothesis that fire plays a role in coastal dune destabilisation. Fires are commonly suggested to have contributed to widespread dune reactivation in Australia and globally, a hypothesis that is relatively untested. We used data from the Landsat Thematic Mapper, Enhanced Thematic Mapper Plus, and Operational Land Imager missions to monitor changes in surface coverage on coastal sand dunes in south-west WA after fires. We analysed 31 fire scars from 1988 to 2016 in two Landsat scenes on the west and south coast of WA. Recovery ratios derived from the Normalised Difference Vegetation Index (NDVI) were used to monitor patterns in post-fire biomass and surface cover. Recovery ratios are correlated with indices of bum severity, and meteorological data to investigate relationships. We also used Maximum Likelihood Classification to monitor changes in bare sand area. Results suggest that recovery followed a strongly consistent pattern, and is characterised by rapid vegetation cover re-establishment within six to twelve months. Prior to this, some aeolian activity may have occurred but without substantial surface changes. Initial germination and/or resprouting were followed by steady growth up to seven years, where NDVI typically neared pre-fire values. Some variation in early recovery occurred between the west and south coast, possibly owing to relative proportions of reseeding and resprouting plants. A log regression explained 75% of the recovery pattern (79% on the south coast). Precipitation had some ability to explain recovery up to nine months post-fire (r(2) = 029 to 0.54). No relationships were observed between estimates of bum severity and recovery. After nine months, the biggest cause of spatial variation in recovery was the pre-fire community composition and related seedbank or resprouting density. Image classification did not identify any new blowout features except where fires were not the primary cause. Results suggest that fires are not presently contributing to the destabilisation of coastal dunes in south-west WA. (C) 2017 Elsevier B.V. All rights reserved.
机译:本研究旨在通过生态-地貌-气候相互作用来确定西澳大利亚州沿海沙丘在数十年时间尺度上对火灾的一般反应,以检验火灾在沿海沙丘失稳中起作用的假设。通常认为,起火是导致澳大利亚和全球沙丘恢复活跃的原因,这一假设尚未得到验证。我们使用Landsat专题测绘仪,Enhanced Thematic Mapper Plus和Operational Land Imager任务中的数据来监测火灾后西南西南沿海沙丘的表面覆盖变化。我们分析了1988年至2016年之间西澳大利亚州西海岸和南海岸的两个Landsat场景中的31个火灾疤痕。从归一化植被指数(NDVI)得出的回收率用于监测火灾后生物量和表面覆盖的模式。回收率与烧伤严重程度指数和气象数据相关联以研究关系。我们还使用了最大似然分类法来监视裸砂区域的变化。结果表明,恢复遵循强烈一致的模式,其特征是在六到十二个月内迅速恢复了植被。在此之前,可能已经发生了一些风沙活动,但没有实质性的表面变化。最初的发芽和/或重新萌发,然后稳定生长长达七年,其中NDVI通常接近射击前的值。西海岸和南海岸之间发生了早期恢复的一些变化,这可能是由于重新播种和重新发芽的植物的相对比例所致。对数回归解释了75%的恢复模式(南海岸为79%)。降水有一定的能力来解释火灾后长达9个月的恢复情况(r(2)= 029至0.54)。烧伤严重程度与恢复之间的关系未发现任何相关性。 9个月后,恢复空间变化的最大原因是火灾前的群落组成和相关的种子库或发芽密度。图像分类没有识别出任何新的井喷特征,除非火灾不是主要原因。结果表明,大火目前并未助长西澳西南部沿海沙丘的不稳定。 (C)2017 Elsevier B.V.保留所有权利。

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