首页|阿蒙森海西部陆架边缘冰山犁沟的形态特征及影响因素研究

阿蒙森海西部陆架边缘冰山犁沟的形态特征及影响因素研究

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冰山犁沟作为典型的冰山侵蚀地貌,其形态特征和影响因素研究涉及冰山的形态、龙骨深度和漂移方向,有助于了解冰架边缘裂解的历史和动态。本文通过解译南极阿蒙森海西部陆架边缘的高精度多波束水深地形,发现了大量的冰山犁沟,并运用V指数模型,分析了冰山犁沟与波纹脊的形态与分布特征,统计了冰山犁沟的走向、长度以及沟内波纹脊的脊高度和脊间距,对其影响因素进行了探讨。冰山犁沟的宽深比、V 指数大小以及横截剖面形态特征很好地指示了形成犁沟的冰山龙骨的尺寸与形状,表明研究区内所有冰山犁沟主体走向为 NEE—SWW,较完整犁沟主体走向为 NE,主要与向陆架外缘流动的沿岸流有关;部分较长犁沟走向为 NW,主要与向西沿岸流、偏东下降风或南极陆坡流有关。冰山犁沟 V 指数平均值为0。132,中位数为 0。121,其宽深比平均值为 32。33,中位数为 27。37。较小的宽深比和V指数表明,冰山犁沟的形成主要与小尺寸的冰山有关,冰山龙骨较深、较尖锐。冰山犁沟内部或者边缘分布着波纹脊微地貌,脊高度为0。1~5。7 m,平均脊高度为2。0 m,脊间距为10~288 m,主要由成组冰山受潮汐上下垂直作用在冰山后缘堆积沉积物形成。
Morphological characteristics and influencing factors of iceberg furrows on the western Amundsen Sea continental shelf margin
Iceberg furrow is a typical iceberg erosion landform,and its morphological characteristics and influ-encing factors are related to iceberg morphology,keel depth and drift direction,which is helpful to under-stand the history and dynamics of ice shelf edge cracking.In this paper,a large number of iceberg furrows were discovered by interpreting the high-precision multi-beam water depth topography of the western Amundsen Sea shelf in Antarctica.The shape and distribution characteristics of iceberg furrows and corru-gation ridge were analyzed by using the V-index model.The strike and length of iceberg furrows and the ridge height and ridge spacing of the corrugation ridge in the ridge were calculated,and the influencing fac-tors were discussed.The width-depth ratio of iceberg furrows,the size of V-index and the morphological characteristics of the cross section can well indicate the size and shape of the iceberg keel that formed the furrows,indicating that the main strike of all iceberg furrows in the study area is NEE—SWW,and the main strike of the intact upper furrows is NE,which is mainly related to the coastal current flowing to the outer edge of the shelf.Part of the longer furrow strike is NW,which is mainly related to westward coastal current,easterly downwind or Antarctic continental slope current.The average V-index of iceberg furrow was 0.132 and the median was 0.121,and the average width-depth ratio was 32.33 and the median was 27.37.The smaller width-to-depth ratio and V-index indicate that the formation of iceberg furrows is mainly associated with smaller icebergs with deeper,sharper keels.The corrugation ridges are distributed in the interior or edge of furrows,the ridge height ranges from 0.1 to 5.7 m,the average ridge height is 2.0 m,and the ridge spacing is 10 to 288 m.The analysis shows that the formation is mainly caused by the accumulation of sediments on the back edge of icebergs under the vertical action of tides.

iceberg furrowiceberg keelmorphological characteristics and influencing factorsAmundsen Sea

赵宁、高金耀、马朋云、韩喜彬、孙曦、阳凡林、葛倩、董超、陆晓鸣、杨春国

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山东科技大学测绘与空间信息学院,山东 青岛 266590

自然资源部海底科学重点实验室,浙江 杭州 310012

自然资源部第二海洋研究所,浙江 杭州 310012

自然资源部海洋环境探测技术与应用重点实验室,广东 广州 510300

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冰山犁沟 冰山龙骨 形态特征及影响因素 阿蒙森海

2024

极地研究
国家海洋局极地考察办公室 中国极地研究中心

极地研究

CSTPCD北大核心
影响因子:0.638
ISSN:1007-7073
年,卷(期):2024.36(4)