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Surface temperature as an indicator of plant species diversity and restoration in oak woodland

机译:表面温度作为橡木林地植物物种多样性和恢复的指标

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摘要

As ecological restoration projects increase in size and complexity, scalable indicators of biodiversity change are needed for monitoring and evaluation. Through three experiments, we tested (1) if relative surface temperature decreased over time across 31 fields initially restored from agriculture to oak woodland between 2006 and 2013, (2) if diurnal temperature variation decreased with time since restoration for the same fields, and (3) if plant species diversity affects relative surface temperature change when controlling for biomass and shade.Thermal imagery was acquired from Landsat satellites 5, 7 and 8 for each growing season in 2002-2018 (excluding 2012) and from the ECOSTRESS thermal instrument on the International Space Station (ISS) for 2018. Three of the 31 fields were surveyed annually 2007-2018 for plant species diversity, ground and canopy cover, and number of woody stems. All surface temperatures were measured in percentage difference relative to adjacent mature forest areas that exhibited stable temperature responses over time.We found (1) a mean decrease in temperature of 1.5 percentage point per year since restoration; (2) a decrease of 4 percentage points of diurnal temperature difference per year since restoration for the same fields; and (3) when controlling for ground and canopy cover, stem count, and Normalized Difference Vegetation Index, an increase of one 'effective number' of plant species diversity decreased relative temperature by 5 percentage points. These results correspond to a decrease of daytime temperature of 4.5 degrees C over 12 years, a decrease of diurnal temperature variation of 5 degrees C in 8 years and a 0.3 degrees C decrease per extra plant species.Our results offer compelling evidence that relative temperature has potential to be used as an indicator to measure ecosystem change resulting from restoration.
机译:由于生态修复项目的规模和复杂性增加,监测和评估需要可扩展的生物多样性变化指标。通过三个实验,我们测试(1)如果在2006年至2013年最初从农业到2006年至2013年之间的31个领域的相对表面温度随着时间的推移而降低,(2),如果随着时间的时间增加,因此在恢复的时间下降,并且( 3)如果植物物种多样性在控制生物量和遮阳篷时影响相对表面温度变化。在2002 - 2018年(不包括2012年)和来自Ecostress热仪器上,从Landsat Satellites 5,7和8获取了热卫星5,7和8的热量图像。 2018年国际空间站(ISS)。31个字段中的三个田地每年调查2007 - 2018年植物物种多样性,地面和遮篷覆盖,木质茎数。所有表面温度均以相对于相邻成熟的森林区域的百分比差,随着时间的推移而表现出稳定的温度响应。我们发现(1)自恢复以来每年的12点百分点的平均降低; (2)每年减少4个百分点的日间温差,因为恢复相同的领域; (3)控制地面和冠层覆盖,茎计数和归一化差异植被指数时,植物物种多样性的一个“有效数”的增加将相对温度降低5个百分点。这些结果对应于12年减少4.5摄氏度的日间温度,8岁的日温度变化的降低,每种额外植物物种减少0.3摄氏度。结果提供了相对温度的令人信服的证据潜力用作衡量恢复产生的生态系统变化的指标。

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