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Regionalization of methane emissions in the Amazon Basin with microwave remote sensing

机译:利用微波遥感对亚马逊盆地甲烷排放进行分区

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摘要

sWetlands of the Amazon River basin are globally significant sources of atmospheric methane. Satellite remote sensing (passive and active microwave) of the temporally varying extent of inundation and vegetation was combined with field measurements to calculate regional rates of methane emission for Amazonian wetlands. Monthly inundation areas for the fringing floodplains of the mainstem Solimoes/Amazon River were derived from analysis of the 37 GHz polarization difference observed by the Scanning Multichannel Microwave Radiometer from 1979 to 1987. L-band synthetic aperture radar data (Japanese Earth Resources Satellite-1) were used to determine inundation and wetland vegetation for the Amazon basin (<500 m elevation) at high (May-June 1996) and low water (October 1995). An extensive set of measurements of methane emission is available from the literature for the fringing floodplains of the central Amazon, segregated into open water, flooded forest and floating macrophyte habitats. Uncertainties in the regional emission rates were determined by Monte Carlo error analyses that combined error estimates for the measurements of emission and for calculations of inundation and habitat areas. The mainstem Solimoes/Amazon floodplain (54-70degreesW) emitted methane at a mean annual rate of 1.3 Tg C yr(-1), with a standard deviation (SD) of the mean of 0.3 Tg C yr(-1); 67% of this range in uncertainty is owed to the range in rates of methane emission and 33% is owed to uncertainty in the areal estimates of inundation and vegetative cover. Methane emission from a 1.77 million square kilometers area in the central basin had a mean of 6.8 Tg C yr(-1) with a SD of 1.3 Tg C yr(-1). If extrapolated to the whole basin below the 500 m contour, approximately 22 Tg C yr(-1) is emitted; this mean flux has a greenhouse warming potential of about 0.5 Pg C as CO2. Improvement of these regional estimates will require many more field measurements of methane emission, further examination of remotely sensed data for types of wetlands not represented in the central basin, and process-based models of methane production and emission.
机译:亚马逊河流域的湿地是全球重要的大气甲烷来源。利用卫星遥感技术(被动和主动微波)将淹没和植被在时间上的变化程度与野外测量相结合,以计算亚马逊湿地甲烷排放的区域速率。 1979年至1987年,通过扫描多通道微波辐射计观测到的37 GHz极化差异,得出了主干Solimoes /亚马逊河边缘洪泛区的每月淹没面积。L波段合成孔径雷达数据(日本地球资源卫星1 )用来确定高水位(1996年5月至6月)和低水位(1995年10月)亚马逊河盆地(海拔500 m以下)的淹没和湿地植被。从文献中可以找到关于亚马逊河中部边缘洪泛区的甲烷排放量的广泛测量结果,这些平原被划分为开阔水域,淹没的森林和漂浮的大型植物栖息地。区域排放率的不确定性是由蒙特卡洛误差分析确定的,该分析结合了误差估计,用于排放量的测量以及淹没和栖息地面积的计算。 Solimoes / Amazon洪泛区主干(54-70华氏度)以平均每年1.3 Tg C yr(-1)的速率排放甲烷,标准偏差(SD)为0.3 Tg C yr(-1)的平均值。该不确定性范围的67%归因于甲烷排放速率的范围,而33%归因于淹没和植物覆盖面积估算的不确定性。中部盆地177万平方公里区域的甲烷排放平均值为6.8 Tg C yr(-1),SD为1.3 Tg C yr(-1)。如果将其外推至等高线以下500 m的整个盆地,则将发射约22 Tg C yr(-1)。该平均通量具有以CO2计约0.5 Pg C的温室变暖潜能。改善这些区域估计值将需要更多的甲烷排放量现场测量,对遥感数据的进一步检查,以了解中部盆地中没有的湿地类型,以及基于过程的甲烷产生和排放模型。

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