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Investigations of the seasonally oscillating sea-ice edge over the Southern Ocean based on Oceansat-1 MSMR and QuikSCAT observations

机译:基于Oceansat-1 MSMR和QuikSCAT观测资料的南大洋季节性海冰边缘调查

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Characterising and understanding the variability of polar sea ice cover at different time scales is fundamental to our understanding of role of polar regions in global climate change. The large expanse of seasonally oscillating sea-ice cover around Antarctica is physically bounded by the continent on its poleward boundary and dynamically on its equatorward boundary by the strong Antarctic Circumpolar Current. This paper attempts to investigate the seasonal migration of the sea ice edge over the southern ocean between these two extremities, on a monthly scale using data from MSMR - the passive multi-frequency scanning microwave radiometer system onboard Oceansat-1. The location of sea ice edge is derived from weekly averaged MSMR 18- GH_z H-polarisation channel brightness temperature images. Simultaneously available sea-ice information from SSM/I is used to validate the MSMR derived sea-ice parameters and to arrive at a brightness temperature threshold of 130 K to distinguish between sea ice and open water. It is observed that the amplitude of seasonal summer-to-winter N-S traverse of sea ice ranges from a few degrees of latitude to as much as about 15 degrees of latitude in different sectors of the southern Ocean around Antarctica. These amplitudes are largest over the Weddell Sea and Ross Sea regions. Further, the monthly rates of this migration show a non-uniform and oscillatory behaviour over the year and reach as high as 8-10 degrees of latitude per month just prior to the approach of summer and winter conditions. The observed seasonal variability shows connectivity to the behaviour of sea-ice edge over longer time scales. These observations have important implications for sea-ice interaction with climate.Recently, we have also embarked on use of higher-resolution active microwave scatterometer data from QuikSCAT to delineate the sea-ice edge more precisely. Preliminary results of these investigations are included.
机译:表征和了解极地海冰在不同时间尺度上的变异性,对于我们了解极地地区在全球气候变化中的作用至关重要。南极洲周围的季节性海洋冰盖的大范围被南极洲极地洋流物理地限制在其极地边界上的大陆边界,并在其赤道边界上被动态限制。本文尝试使用MSMR(Oceansat-1上的无源多频扫描微波辐射计系统)的数据,每月调查这两个末端之间南部海洋上海冰边缘的季节性迁移。海冰边缘的位置来自每周平均MSMR 18-GH_z H极化通道亮度温度图像。来自SSM / I的同时可用的海冰信息用于验证MSMR得出的海冰参数,并达到130 K的亮度温度阈值,以区分海冰和开阔水域。可以观察到,南极周围南大洋不同区域海冰从夏季到冬季的季节性N-S横移的幅度范围从几个纬度到大约15个纬度。这些振幅在韦德尔海和罗斯海地区最大。此外,这种迁徙的月率在一年中显示出不均匀和波动的行为,并且正好在夏季和冬季条件临近之前达到每月高达8-10度的纬度。观测到的季节变化表明,在较长的时间尺度上,它们与海冰边缘的行为具有连通性。这些观测结果对海冰与气候的相互作用具有重要意义。最近,我们还着手使用来自QuikSCAT的高分辨率有源微波散射仪数据,以更精确地描绘海冰边缘。这些调查的初步结果也包括在内。

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