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Assessment of AMSR-E Antarctic Winter Sea-Ice Concentrations Using Aqua MODIS

机译:使用Aqua MODIS评估AMSR-E南极冬季海冰浓度

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An assessment of the standard Advanced Microwave Scanning Radiometer for the Earth Observing System (AMSR-E) sea-ice concentrations for the Antarctic winter is made from a comparison of nearly 40 000 AMSR-E sea-ice concentration values with geolocated sea-ice concentrations derived from ten Aqua Moderate Resolution Imaging Spectroradiometer (MODIS) scenes acquired on October 1st and 2nd of 2005 and 2006. The standard AMSR-E sea-ice concentration products are produced using the National Aeronautics and Space Administration Team 2 sea-ice algorithm. The ten MODIS scenes cover portions of almost all the sea-ice regions surrounding the Antarctic continent. The AMSR-E averaged ice concentration biases relative to MODIS (AMSR-E minus MODIS) ranged from less than $-$0.5% to $-$ 18%, and the corresponding averaged root-mean-square (rms) errors ranged from 2% to 24%. One scene [October 1, 2006 (0550 UT)] had both the largest bias ($-$18%) and rms error (24%), whereas the other nine scenes had an average bias of $-$ 1.5% and an average rms error of 4.9%. The biases and rms errors are correlated with the fractions of new ice and open water. This is consistent with the findings that the largest errors in ice concentration derived from the AMSR-E occur in the marginal ice zone (MIZ) and along the ice edge and are likely caused by sea-ice flooding in the MIZ and new-ice production at the ice edge.
机译:通过将近40 000 AMSR-E海冰浓度值与地理位置优越的海冰浓度进行比较,对南极冬季地球观测系统(AMSR-E)海冰浓度的标准高级微波扫描辐射计进行了评估。这些数据来自于2005年10月1日和2日以及2006年10月获得的十个Aqua中分辨率成像光谱仪(MODIS)场景。标准AMSR-E海冰浓缩产品是使用美国国家航空航天局第二小组海冰算法生产的。十个MODIS场景涵盖了南极大陆周围几乎所有海冰区域的一部分。 AMSR-E相对于MODIS的平均冰浓度偏差(AMSR-E减去MODIS)的范围从小于$-$ 0.5%到$-$ 18%,并且相应的平均均方根(rms)误差范围为2%至24%。一个场景[2006年10月1日(0550 UT)]具有最大的偏差($-$ 18%)和均方根误差(24%),而其他九个场景的平均偏差为$-$ 1.5%和均方根误差为4.9%。偏差和均方根误差与新冰和开水的分数相关。这与以下发现一致:AMSR-E引起的冰浓度最大误差发生在边缘冰区(MIZ)以及沿冰边缘,并且可能是由于MIZ中的海冰泛滥和新冰生产引起的在冰边。

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