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Estimation of Particulate Organic Carbon in the ocean from space-based polarization lidar measurements

机译:通过空间极化激光雷达测量估算海洋中的微粒有机碳

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A relationship between depolarization ratio and surface concentration of particulate organic carbon (POC) is developed from the NASA SeaWiFS Bio-optical Archive and Storage System (SeaBASS) in situ measurements and the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) active lidar measurements. This relationship provides an algorithm for estimating global POC from satellite or airborne polarization lidar measurements. Application of this relationship to CALIOP data indicates that the estimates of POC ranges from about 3.3 mg/m~3 within the South Pacific Subtropical Gyre to 1.2×10~3 mg/m~3 in the area near land are in good agreement with Moderate Resolution Imaging spectroradiometer (MODIS) POC products. Our results present depolarization ratio as a valuable tool for evaluating global POC predictions in ocean ecosystem. The application of the algorithm to a 7-year of CALIOP depolarization ratio mean values revealed patters of seasonal and interannual variability of POC. By comparing the results averaged over the entire study region and entire season for each year separately, we found that the lowest POC occurred in 2013 and the highest POC occurred in 2008.
机译:NASA SeaWiFS生物光学存档和存储系统(SeaBASS)的原位测量和带正交偏振的云气溶胶激光雷达(CALIOP)主动激光雷达测量开发了去极化率与颗粒有机碳(POC)表面浓度之间的关系。这种关系提供了一种从卫星或机载极化激光雷达测量结果估算全局POC的算法。将这种关系应用于CALIOP数据表明,POC的估计值范围从南太平洋亚热带环流内的大约3.3 mg / m〜3到陆地附近地区的1.2×10〜3 mg / m〜3都与中等分辨率成像光谱仪(MODIS)POC产品。我们的结果表明去极化率是评估海洋生态系统中全球POC预测的有价值的工具。该算法在7年的CALIOP去极化率平均值中的应用揭示了POC的季节和年际变化规律。通过分别比较整个研究区域和整个季节每年的平均结果,我们发现最低的POC发生在2013年,最高的POC发生在2008年。

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