首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Assessing the impact of brightness temperature simulation adjustment conditions in correcting Metop-A SST over the Mediterranean Sea
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Assessing the impact of brightness temperature simulation adjustment conditions in correcting Metop-A SST over the Mediterranean Sea

机译:评估亮度温度模拟调整条件对校正地中海上的Metop-A SST的影响

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Multispectral sea surface temperature (SST) algorithms applied to infrared (IR) radiometer data exhibit regional biases due to the intrinsic inability of the SST algorithmto cope with the vast range of atmospheric types, mainly influenced by water vapor and temperature profiles. Deriving a SST correction from simulated brightness temperatures (BTs), obtained by applying a Radiative Transfer Model (RTM) to Numerical Weather Prediction (NWP) atmospheric profiles and first guess SST, is one of the solutions to reduce regional biases. This solution is envisaged in the particular case of Metop-A Advanced Very High Resolution Radiometer (AVHRR) derived SST. Simulated BTs show errors, linked to RTM, atmospheric profiles or guess field errors. We investigated the conditions of adjusting simulated to observed BTs in the particular case of the Mediterranean Sea over almost one year. Our study led to define optimal spatio/temporal averaging parameters of the simulation observation differences, both during day and night, summer and colder season and for two simulation modes: operational (with reduced vertical resolution – 15 levels – NWP atmospheric profiles and two days old analysis used as first guess SST) and delayed (full vertical resolution – 91 levels – and concurrent analysis used as first guess SST). Each BT adjustment has been evaluated by comparing the corresponding corrected AVHRR SST to the AATSR SST that weadopted as validation reference.We obtained an optimized result across all defined conditions and modes for a spatial smoothing of 15 deg and a temporal averaging between 3 and 5 days. Specifically, analyses based on 10 day averages showed that a standard deviation based criterion favors spatial smoothing above 10 deg for all temporal averaging, while a bias based criterion favors shorter temporal averaging during daytime (b 5 days) and higher spatial smoothing (N10 deg) for nighttime. This study has shown also the impact of diurnal warming both in deriving BT adjustment and in validation results.
机译:由于SST算法固有的能力无法应对主要受水蒸气和温度曲线影响的各种大气类型,因此应用于红外(IR)辐射计数据的多光谱海面温度(SST)算法表现出区域偏差。通过将辐射传递模型(RTM)应用于数值天气预报(NWP)大气廓线和首先猜测SST,从模拟亮度温度(BTs)得出SST校正是减少区域偏差的解决方案之一。在Metop-A先进超高分辨率辐射计(AVHRR)衍生的SST的特殊情况下,可以设想此解决方案。模拟的BT会显示与RTM相关的错误,大气廓线或猜测场错误。我们研究了在将近一年的特定情况下,对地中海特定情况下的模拟BT进行调整的条件。我们的研究确定了白天和黑夜,夏季和寒冷季节以及两种模拟模式下模拟观测差异的最佳时空平均参数:可操作(垂直分辨率降低– 15级– NWP大气廓线和两天龄)分析用作第一猜测SST)和延迟(全垂直分辨率-91级-并发分析用作第一猜测SST)。通过将相应的校正后的AVHRR SST与我们用作验证参考的AATSR SST进行比较,对每个BT调整进行了评估。我们在所有定义的条件和模式下获得了优化的结果,空间平滑度为15度,时间平均为3-5天。具体而言,基于10天平均值的分析表明,对于所有时间平均而言,基于标准偏差的标准都有利于10度以上的空间平滑,而对于白天(b 5天)而言,基于偏差的标准则有利于较短的时间平均,而较高的空间平滑度(N10度)晚上这项研究还显示了昼夜升温对推导BT调整和验证结果的影响。

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