首页> 外文会议>Imaging a Sustainable Future >ASSESSMENT OF SEA ICE FREEBOARD AND THICKNESS IN MCMURDO SOUND, ANTARCTICA, DERIVED BY GROUND VALIDATED SATELLITE ALTIMETER DATA
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ASSESSMENT OF SEA ICE FREEBOARD AND THICKNESS IN MCMURDO SOUND, ANTARCTICA, DERIVED BY GROUND VALIDATED SATELLITE ALTIMETER DATA

机译:在McMurdo,Antarctica中评估海冰干舷和厚度,由地面验证的卫星高度计数据衍生

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This investigation employs the use of ICESat to derive freeboard measurements in McMurdo Sound in the western Ross Sea, Antarctica, for the time period 2003-2009. Methods closely follow those previously presented in the literature but are complemented by a good understanding of general sea ice characteristics in the study region from extensive temporal ground investigations but with limited spatial coverage. The aim of remote sensing applications in this area is to expand the good knowledge of sea ice characteristics within these limited areas to the wider McMurdo Sound and western Ross Sea region. The seven year Austral Spring (September, October, and November) investigation is presented for sea ice freeboard alone. An interannual comparison of mean freeboard indicates an increase in multiyear sea ice freeboard from 1.08 m in 2003 to 1.15 m in 2009 with positive and negative variation in between. No significant trend was detected for first year sea ice freeboard. Further, an Envisat imagery investigation complements the freeboard assessment. The multiyear sea ice was observed to increase by 254 % of its original 2003 area, as firstyear sea ice persisted through the 2004 melt season into 2005. This maximum coverage then gradually diminished by 2009 to 20 % above the original 2003 value. The mid study period increase is likely attributed to the passage of iceberg B-15A minimising oceanic pressures and preventing sea ice breakout in the region.
机译:该调查采用ICESAT在2003 - 2009年时间期间使用ICESAT在西罗斯海,南极洲南极洲的McMurdo声音中的空间测量。方法密切关注先前在文献中呈现的那些,但是通过广泛的颞地调查,良好地了解研究地区的一般海冰特征,但空间覆盖率有限。该领域遥感应用的目的是扩大这些有限地区内海冰特性的良好知识,以更广泛的McMurdo声音和西罗海地区。单独为海冰干舷提供七年澳大利亚春季(9月,10月和11月)调查。平均收油板的续比比较表明,2003年的1.08米的多年海冰干冰板增加到2009年的1.15米,与之间的正面和负变化。对第一年海冰滑动机没有检测到显着趋势。此外,Envisat Imagery Checulations补充了收集的游泳池评估。由于2004年融化季节持续到2005年,近年的2003年普遍存在的2003年,多年海冰增加了254%。随后,这一最大覆盖率将逐渐减少到2009年以上原始2003年上方20%。中学期间的增加可能归因于冰山B-15A通过最小化海洋压力和预防该地区的海冰突破。

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