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Comparison of CryoSat-2 and ENVISAT radar freeboard over Arctic sea ice: toward an improved Envisat freeboard retrieval

机译:北极海冰上CryoSat-2和ENVISAT雷达干舷的比较:改进的Envisat干舷检索

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pstrongAbstract./strong Over the past decade, sea-ice freeboard has been monitored with various satellite altimetric missions with the aim of producing long-term time series of ice thickness. While recent studies have demonstrated the capacity of the CryoSat-2 mission (2010a??present) to provide accurate freeboard measurements, the current estimates obtained with the Envisat mission (2002a??2012) still require some large improvements. brbr In this study, we first estimate Envisat and CryoSat-2 radar freeboard by using the exact same processing algorithms. We then analyse the freeboard difference between the two estimates over the common winter periods (November 2010a??April 2011 and November 2011a??March 2012). The analysis of along-track data and gridded radar freeboard in conjunction with Envisat pulse-peakiness (PP) maps suggests that the discrepancy between the two sensors is related to the surface properties of sea-ice floes and to the use of a threshold retracker. brbr Based on the relation between the Envisat pulse peakiness and the radar freeboard difference between Envisat and CryoSat-2, we produce a monthly CryoSat-2-like version of Envisat freeboard. The improved Envisat data set freeboard displays a similar spatial distribution to CryoSat-2 (RMSDspan class="thinspace"/spana??=a??span class="thinspace"/span1.5span class="thinspace"/spancm) during the two ice growth seasons and for all months of the period of study. brbr The comparison of the altimetric data sets with in situ ice draught measurements during the common flight period shows that the improved Envisat data set (RMSEspan class="thinspace"/spana??=a??span class="thinspace"/span12a??28span class="thinspace"/spancm) is as accurate as CryoSat-2 (RMSEspan class="thinspace"/spana??=a??span class="thinspace"/span15a??21span class="thinspace"/spancm) and much more accurate than the uncorrected Envisat data set (RMSEspan class="thinspace"/spana??=a??span class="thinspace"/span178a??179span class="thinspace"/spancm). brbr The comparison of the improved Envisat radar freeboard data set is then extended to the rest of the Envisat mission to demonstrate the validity of PP correction from the calibration period. The good agreement between the improved Envisat data set and the in situ ice draught data set (RMSEspan class="thinspace"/spana??=a??span class="thinspace"/span13a??32span class="thinspace"/spancm) demonstrates the potential of the PP correction to produce accurate freeboard estimates over the entire Envisat mission lifetime./p.
机译:> >摘要。在过去的十年中,海冰干舷已经通过各种卫星测高任务进行了监视,目的是产生长期的冰厚时间序列。尽管最近的研究表明CryoSat-2任务(2010a-至今)提供准确的干舷测量的能力,但通过Envisat任务(2002a-2012)获得的当前估算值仍需要进行一些较大的改进。 在这项研究中,我们首先使用完全相同的处理算法来估算Envisat和CryoSat-2雷达干舷。然后,我们分析了共同冬季(2010年11月至2011年4月和2011年11月至2012年3月)两个估算值之间的干舷差异。结合Envisat脉冲峰值(PP)地图对沿航迹数据和栅格化的雷达干舷的分析表明,这两个传感器之间的差异与海冰絮凝物的表面特性以及阈值跟踪器的使用有关。 根据Envisat脉冲峰值与Envisat和CryoSat-2之间的雷达干舷差异之间的关系,我们每月制作一次类似CryoSat-2的Envisat干舷版本。改进的Envisat数据集干舷显示出与CryoSat-2类似的空间分布(RMSD class =“ thinspace”> a ?? = a ?? class =“ thinspace”> 1.5 <在两个冰的生长季节以及研究期间的所有月份中,均需输入span class =“ thinspace”> cm)。 在常规飞行期间将高空数据集与原位冰吃水测量值进行比较,结果表明改进后的Envisat数据集(RMSE class =“ thinspace”> a ?? = a ?? class =“ thinspace”> 12a ?? 28 class =“ thinspace”> cm)的精度与CryoSat-2(RMSE class =“ thinspace”> < / span> a ?? = a ?? class =“ thinspace”> 15a ?? 21 class =“ thinspace”> cm),并且比未校正的Envisat数据集更准确(RMSE class =“ thinspace”> a ?? = a ?? class =“ thinspace”> 178a ?? 179 class =“ thinspace”> cm )。 然后,将改进的Envisat雷达干舷数据集的比较扩展到Envisat任务的其余部分,以证明在校准期间PP校正的有效性。改进的Envisat数据集和现场冰吃水数据集之间的良好一致性(RMSE class =“ thinspace”> a ?? = a ?? class =“ thinspace”> 13a ?? 32 class =“ thinspace”> cm)演示了PP校正在整个Envisat任务寿命内产生准确的干舷估计值的潜力。

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