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Estimating release of carbon from forest fires in Alaska using satellite remote sensing data

机译:使用卫星遥感数据估算阿拉斯加州森林火灾碳的释放

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While there is little doubt the fossil fuel burning has led to increases in the atmospheric concentration of CO/sub 2/ over the past century, analyses show this increase is significantly less than the total amount of CO/sub 2/ released into the atmosphere through this burning. Studies have shown that other human practices (land clearing and biomass burning) have released significant amounts of carbon into the atmosphere (Houghton 1991). In addition, terrestrial and aquatic biomes act as sources and sinks for atmospheric carbon based upon a complex set of biological, chemical and physical processes. To accurately predict future trends in the rise in atmospheric CO/sub 2/ requires developing a better understanding of the terrestrial and oceanic sources and sinks of carbon. Approximately 4 Pg C yr/sup -1/ are released into the atmosphere during the burning of biomass. In tropical regions Houghton (1991) estimates there is a net release of C to the atmosphere due to burning of biomass in cleared forest lands. When considering biomass burning on a global scale, researchers have discounted the role of fire in boreal forests. However, several oversights were made in these earlier studies. First, the total area burned in boreal forests was significantly underestimated, by as much as an order of magnitude. Second, these initial studies focused on the burning of aboveground biomass, ignoring the large amounts of organic matter in the ground layer that are consumed during fires in boreal forests. Studies have indicated that fires in boreal forests could become a significant source of carbon to the atmosphere over the next half century. Several researchers have demonstrated that low resolution satellite imagery from NOAA's AVHRR system can be used to map and locate fires in Russian and Alaskan boreal forests. In this paper, the authors develop a ground-based model of biomass levels and carbon-release during fires in Alaskan boreal forests to estimate the amounts of carbon released during fire in this region for 1990 and 1991. The authors use the location and areal extent of fires throughout Alaska in 1990 and 1991 derived from AVHRR data.
机译:虽然毫无疑问,化石燃料燃烧导致了在过去的世纪中的大气浓度的大气浓度增加,但分析显示这种增加明显小于通过释放到大气中的CO / SUM 2 /释放到大气中的总量这种燃烧。研究表明,其他人类实践(陆地清算和生物质燃烧)已将大量碳释放到大气中(Houghton 1991)。此外,基于复杂的生物学,化学和物理过程,陆地和水生生物体作为大气碳的来源和水槽。为了准确地预测大气中的CO / SUB中的未来趋势/需要更好地了解陆地和海洋来源和碳的汇。在生物质燃烧期间,大约4pg C YR / SUP -1 /释放到大气中。在热带地区,霍顿(1991)估计由于在清除林地中的生物质燃烧,净释放到大气中。考虑到全球规模燃烧生物量,研究人员在北方森林中折扣着火灾的作用。然而,在这些早期的研究中进行了若干监督。首先,在北方森林中燃烧的总面积显着低估,低于数量级。其次,这些初步研究侧重于地上生物质的燃烧,忽略了在北部森林中消耗期间消耗的地层中的大量有机物。研究表明,在未来半个世纪,北方森林的火灾可能成为大气的重要碳源。几位研究人员已经证明,NOAA的AVHRR系统的低分辨率卫星图像可用于绘制和定位俄罗斯和阿拉斯加博林林的火灾。在本文中,作者在阿拉斯加博林斯的火灾中开发了基于地基的生物量水平和碳释放,以估计1990年和1991年在该地区的火灾中释放的碳量。作者使用了地理位置和面积1990年和1991年的阿拉斯加州的火灾来自AVHRR数据。

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