沙丘大小不对称表明沙丘生长受基底面积或体积控制

IF 2.8 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL Earth Surface Processes and Landforms Pub Date : 2024-05-08 DOI:10.1002/esp.5876
Dominic T. Robson, Andreas C. W. Baas
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引用次数: 0

摘要

我们引入了一个新的分析模型,从沙丘的两侧来分析沙丘的生长过程,并由此推导出在三种不同机制主导生长过程的情况下,沙丘双侧不对称的大小依赖性表达式。对火星和地球上沙丘形态的分析表明,不对称分布可能存在两种不同的吸引状态。通过将我们的分析结果与观测结果进行比较,我们发现沙丘的生长似乎是由与基底面积或基底体积成正比的过程主导的,而不是像通常假设的那样与基底宽度成线性关系。我们提出了一些假设,以解释风力多变导致的面积主导型增长和碰撞导致的体积主导型增长。这些预测似乎与现有的陆地蜂群和类似于巴歇尔沙丘的海底海床形态的数据相吻合,并提供了根据沙丘形态数据预测难以接近的风机制模式的可能性。
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Size‐dependent asymmetry of barchans indicates dune growth controlled by basal area or bulk volume
We introduce a novel analytical model of the growth of barchan dunes in terms of their two flanks, from which we derive expressions for the size‐dependence of the bilateral asymmetry of these bedforms in three cases where different mechanisms dominate the growth process. Analysis of the morphology of barchans on Mars and Earth suggest that there may exist two distinct attractor states for the asymmetry distribution. By comparing our analytical results with the observations, we show that the growth of barchan dunes appears to be dominated by processes, which are proportional to the basal area or volume of the bedforms, rather than being linear to their width as is typically assumed. We propose hypotheses explaining area‐dominated growth as a result of variable wind regimes and volume‐dominated growth from collisions. These predictions appear to be in line with the available data for the terrestrial swarms and barchan‐like submarine bedforms and offer the potential of predicting patterns in inaccessible wind regimes from data on the morphology of the dunes.
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来源期刊
Earth Surface Processes and Landforms
Earth Surface Processes and Landforms 地学-地球科学综合
CiteScore
6.40
自引率
12.10%
发文量
215
审稿时长
4 months
期刊介绍: Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with: the interactions between surface processes and landforms and landscapes; that lead to physical, chemical and biological changes; and which in turn create; current landscapes and the geological record of past landscapes. Its focus is core to both physical geographical and geological communities, and also the wider geosciences
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