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A practical method for simulating AVHRR-consistent NDVI data series using narrow MODIS channels in the 0.5-1.0 /spl mu/m spectral range

机译:在0.5-1.0 / spl mu / m光谱范围内使用窄MODIS通道模拟AVHRR一致性NDVI数据序列的实用方法

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Over the past two decades, a key indicator of climate change has been the long time series of global maps of the normalized difference vegetation index (NDVI), derived from remotely sensed data acquired with a series of NOAA advanced very high resolution radiometer (AVHRR) instruments from space. These NDVI values are calculated from relatively broad AVHRR channels in the red and near-infrared regions. Continuation of this long term data set is extremely valuable for climate-related research, However, sometime in the coming decade, the AVHRR time series measurements will no longer be continued. Instead, the measurements will be made using newer generation satellite instruments having narrower channels and improved spatial resolution. For example, the moderate resolution imaging spectroradiometer (MODIS) onboard the Terra spacecraft has several narrow channels in the 0.4-1.0 spectral range. The NDVI values derived from the MODIS red channel and near-IR channel will be biased compared to those derived from the broader AVHRR channels because of differences in channel positions and widths for the two instruments. The narrow MODIS near-IR channel is only slightly affected by atmospheric water vapor absorption, while the broad AVHRR near-IR channel is strongly affected by water vapor absorption. As a result, the largest bias comes from the near-IR channels on the two instruments. To a lesser extent, the bias also comes from the differences between the red channel positions and the widths of MODIS and AVHRR instruments. In this paper, the authors describe a practical method for simulating AVHRR NDVI values using several narrower MODIS channels in the 0.4-1.0 /spl mu/m spectral range, including the MODIS green channel and the water vapor absorption channel.
机译:在过去的二十年中,气候变化的关键指标是标准化序列差异植被指数(NDVI)的长期全球地图,这些序列是通过使用一系列NOAA先进超高分辨率辐射计(AVHRR)获取的遥感数据得出的太空中的乐器。这些NDVI值是根据红色和近红外区域中相对较宽的AVHRR通道计算得出的。长期数据集的延续对于与气候相关的研究非常有价值,但是,在未来十年的某个时候,AVHRR时间序列的测量将不再继续。相反,将使用具有更窄通道和更高空间分辨率的新一代卫星仪器进行测量。例如,Terra航天器上的中分辨率成像光谱仪(MODIS)在0.4-1.0光谱范围内有几个狭窄的通道。与从较宽的AVHRR通道获得的NDVI值相比,从MODIS红色通道和近红外通道获得的NDVI值将存在偏差,因为这两种仪器的通道位置和宽度不同。狭窄的MODIS近红外通道仅受大气中水蒸气吸收的轻微影响,而较宽的AVHRR近红外通道则受水蒸气吸收的强烈影响。结果,最大的偏差来自两台仪器的近红外通道。在较小程度上,偏差还来自红色通道位置与MODIS和AVHRR仪器宽度之间的差异。在本文中,作者描述了一种使用0.4-1.0 / spl mu / m光谱范围内的几个较窄的MODIS通道(包括MODIS绿色通道和水蒸气吸收通道)来模拟AVHRR NDVI值的实用方法。

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