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Using limited time period trends as a means to determine attribution of discrepancies in microwave sounding unit–derived tropospheric temperature time series

机译:使用有限的时间趋势来确定微波探测单位衍生的对流层温度时间序列中差异的原因

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Limited time period running trends are created from various microwave sounding unit (MSU) difference time series between the University of Alabama in Huntsville and Remote Sensing System (RSS) group's lower troposphere (LT) and mid troposphere to lower stratosphere channels. This is accomplished in an effort to determine the causes of the greatest discrepancies between the two data sets. Results indicate the greatest discrepancies were over time periods where NOAA 11 through NOAA 15 adjustments were applied to the raw LT data over land. Discrepancies in the LT channel are shown to be dominated by differences in diurnal correction methods due to orbital drift; however, discrepancies from target parameter differences are also present. Comparison of MSU data with the reduced Radiosonde Atmospheric Temperature Products for Assessing Climate radiosonde data set indicates that RSS's method (use of climate model) of determining diurnal effects is likely overestimating the correction in the LT channel. Diurnal correction signatures still exist in the RSS LT time series and are likely affecting the long-term trend with a warm bias. Our findings enhance the importance of understanding temporal changes in the atmospheric temperature trend profile and their implications on current climate studies.
机译:有限的时间段运行趋势是由汉斯维尔的阿拉巴马大学与遥感系统(RSS)组的低对流层(LT)和对流层中至低平流层通道之间的各种微波测深单元(MSU)时差序列创建的。这是为了确定两个数据集之间最大差异的原因而完成的。结果表明最大的差异是在一段时间内,将NOAA 11至NOAA 15调整应用于陆地上的原始LT数据。由于轨道漂移,昼夜校正方法的差异主要表现为LT通道的差异。但是,也存在与目标参数差异的差异。 MSU数据与用于评估气候无线电探空仪数据集的降低的探空仪大气温度产品的比较表明,RSS的确定昼夜影响的方法(使用气候模型)可能高估了LT通道中的校正。昼夜校正信号仍然存在于RSS LT时间序列中,并且可能会以温暖的偏见影响长期趋势。我们的发现提高了理解大气温度趋势分布的时间变化及其对当前气候研究的影响的重要性。

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