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Antarctic sea-ice extents and concentrations:comparison of satellite and ship measurements from International Polar Year cruises

机译:南极海冰范围和浓度:国际极地年巡游中卫星和船舶测量的比较

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Antarctic Sea Ice Processes and Climate (ASPeCt) ship-based ice observations, conducted during the Sea Ice Mass Balance in the Antarctic (SIMBA) and Sea Ice Physics and Ecosystem eXperiment (SIPEX) International Polar Year (IPY) cruises (September-October 2007), are used to validate remote-sensing measurements of ice extent and concentration. Observations include varied sea-ice types at and inside the ice edge of West (~90° W) and East (~1200 E) Antarctica. Time series of Advanced Microwave Scanning Radiometer-Earth Observing System (AMSR-E) ice extents and US National Ice Center (NIC) ice edges were obtained for the 2007-08 periods bracketing the period these cruises were conducted. A comparison between passive microwave satellite imagery and ASPeCt observations of sea-ice concentration during two cruises was also performed. In 90° W regions, the concentrated pack ice indicated good correlation between ship observations and passive microwave estimates of the ice concentration (R~2 = 0.80). In the marginal zone of West Antarctica and over nearly the entire sea-ice zone of East Antarctica, correlation dropped to R~2 < 0.60. These findings are consistent with other studies comparing passive microwave and ship observations and further verify that the East Antarctic sea-ice zone is more marginal in character. There are significant ice-edge differences between AMSR-E and NIC between late November 2007 and early March 2008 such that the AMSR-E sea-ice extent estimate is 1-2 x 10~6 km~2 less than the NIC estimate.
机译:在南极海冰质量平衡(SIMBA)和海冰物理与生态系统试验(SIPEX)国际极地年(IPY)航行期间进行的南极海冰过程和气候(ASPeCt)船上冰观测(2007年9月至10月) ),用于验证冰范围和浓度的遥感测量。观测结果包括南极西部(〜90°W)和东部(〜1200 E)冰边缘及其内部的各种海冰类型。在2007-08年期间获得了高级微波扫描辐射计-地球观测系统(AMSR-E)的冰范围和美国国家冰中心(NIC)的冰边缘时间序列,这些时间段与进行这些航行的时间段成正比。还对无源微波卫星图像和两次巡航期间海冰浓度的ASPeCt观测值进行了比较。在90°W区域,浓缩冰块表明船舶观测结果与被动微波估计的冰含量之间具有良好的相关性(R〜2 = 0.80)。在南极西部的边缘地区和南极东部的整个海冰区域,相关性下降到R〜2 <0.60。这些发现与其他研究比较被动微波和舰船观测结果是一致的,并进一步证明了南极东部海冰带的特征更为边缘。在2007年11月下旬至2008年3月初之间,AMSR-E和NIC之间存在明显的冰缘差异,因此AMSR-E的海冰范围估计值比NIC估计值少1-2 x 10〜6 km〜2。

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