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Evaluation of television infrared observation satellite (TIROS-N) operational vertical sounder (TOVS) spaceborne CO2 estimates using model simulations and aircraft data

机译:评估电视红外观测卫星(TIROs-N)操作垂直测深仪(TOVs)星载CO 2 使用模型模拟和飞机数据进行估算

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摘要

[1] CO mixing ratio derived from spaceborne measurements of the Television Infrared Observation Satellite (TIROS-N) Operational Vertical Sounder (TOVS) instrument onboard NOAA-10 available for the time period 1987 - 1991 are evaluated against modeling results and aircraft measurements. The model simulations are based on two transport models and two sets of surface fluxes which have been optimized in order to fit near-surface atmospheric CO measurements through a transport model ( using an inverse procedure). In the tropics the zonal mean annual cycle and growth rate of the satellite product are consistent with those of the models. However, north-to-south gradients and spatial distributions for a given month show large differences. There are large regional patterns that can reach 7 ppm in the satellite retrievals ( over regions of a few thousand kilometers wide) but are absent in the model predictions. The root-mean-square (RMS) differences between the models and the satellite product are around 1.7 ppm. One time series of the model CO trend is used to extrapolate to the airborne measurement periods ( 1991 - 2003) both the satellite and the model monthly products to the airborne measurement period. The RMS difference between the airborne measurements and the extrapolated model predictions is around 1 ppm, while it is 2 ppm for the satellite estimate. These comparisons suggest that the large spatial variability of TOVS retrievals reflects substantial regional biases and noise which need to be reduced before remotely sensed CO from TOVS will help constrain our knowledge of the carbon cycle. [References: 43]
机译:[1]根据建模结果和飞机测量结果,评估了NOAA-10上可用的电视红外观测卫星(TIROS-N)垂直操作测深仪(TOVS)仪器在1987年至1991年的空间测量中得出的CO混合比。模型模拟基于两个运输模型和两组表面通量,这些模型已经过优化,以便通过运输模型(使用逆过程)拟合近地表大气CO测量值。在热带地区,卫星产品的纬向平均年周期和增长率与模型的一致。但是,给定月份的南北向梯度和空间分布显示出很大的差异。在卫星检索中(在几千公里宽的区域内)有很大的区域模式可以达到7 ppm,但是在模型预测中却没有。模型与卫星产品之间的均方根(RMS)差异约为1.7 ppm。使用CO趋势模型的一个时间序列来推断机载测量周期(1991年至2003年),同时将卫星和模型月度产品推算到机载测量周期。机载测量值与外推模型预测值之间的RMS差约为1 ppm,而卫星估算值的RMS差为2 ppm。这些比较表明,TOVS取回的较大空间变化反映了较大的区域偏差和噪声,需要减少这些偏差,然后才能从TOVS遥感CO有助于限制我们对碳循环的认识。 [参考:43]

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