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Evaluation of the multichannel sea surface temperature algorithm along the Brazilian coast

机译:评价巴西海岸沿岸沿岸海面温度算法

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The accuracy to which sea surface temperature (SST) can be estimated using satellite infrared radiometers is limited mainly by atmospheric contamination. This work reports an investigation on the global coefficients of the Multichannel Sea Surface Temperature (MCSST) algorithm along the Brazilian coast (8/spl deg/N-36/spl deg/S). MCSST data were evaluated for the period November 1981-December 1986 in conjunction with temperature data from the Comprehensive Ocean-Atmosphere Data Set (COADS). Monthly statistics of 2/spl deg/ bin between satellite and ship SST differences ranged from -3.44/spl deg/ to 2.84/spl deg/C and mean differences from -0.18/spl deg/ to 9.47/spl deg/C (standard deviation from 0.52/spl deg/ to 0.65/spl deg/C). Interannual oscillations of the SST differences were observed along the western Atlantic Ocean and can be partly explained by the 1982-1983 El Nino event.
机译:使用卫星红外辐射仪估计海表面温度(SST)的准确性主要受大气污染的限制。这项工作报告了对巴西海岸(8 / SPL DEG / N-36 / SPL DEG / S)的多通道海表面温度(MCSST)算法的全球系数调查。 MCSST数据于1981年11月至1986年11月期间与来自综合海洋气氛数据集(Coads)的温度数据相结合。卫星和船舶SST差异之间的2 / SPL DEG / BIN的每月统计数据范围为-3.44 / SPL DEG /〜2.84 / SPL DEG / C,与-0.18 / SPL DEG /〜9.47 / SPL DEG / C的平均差异(标准偏差从0.52 / SPL DEG /至0.65 / SPL DEG / C)。沿着西部大西洋观察了SST差异的际振荡,可以部分地解释1982-1983 El Nino事件。

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