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中国沙漠 ›› 2003, Vol. 23 ›› Issue (5): 573-576.

• 研究简报 • 上一篇    下一篇

气流水平涡度对沙纹形成的动力作用

张广兴, 李霞   

  1. 中国气象局 乌鲁木齐沙漠气象研究所, 新疆 乌鲁木齐 830002
  • 收稿日期:2002-09-15 修回日期:2002-10-20 出版日期:2003-10-20 发布日期:2003-10-20
  • 作者简介:张广兴(1963-)男(汉族),甘肃武威人,副研究员,主要从事数值模式和沙漠气象方面的研究。E-mail:zhangguangx@163.com
  • 基金资助:
    科技部社会公益类研究专项"沙尘暴观测及分级标准研究";科技部重大基础研究前期专项(2002CCA04600)资助

Dynamic Functions of Horizontal Airflow Vorticity to Dune Ripples

ZHANG Guang-xing, LI Xia   

  1. Institute of Desert Meteorology, China Metrological Administration, Urumqi 830002, China
  • Received:2002-09-15 Revised:2002-10-20 Online:2003-10-20 Published:2003-10-20

摘要: 从分析沙面流体边界层特征入手,导出了与沙面平行而与气流垂直的水平涡度分量ξy和高度成倒数的关系,说明气流经过沙面是高度有旋的。因此,气流质点在做水平运动的同时做旋转运动,其结果形成类似摆线的波动。不同尺度的波相互叠加,通过自组织形成有序的波动。沙粒在波谷被风蚀,在波峰堆积,最终形成沙波和沙纹。

关键词: 沙纹, 水平涡度, 气流波动

Abstract: Started from the analysis on the boundary characteristics of airflow on dune,an inverse ratio relationship between horizontal vorticity fraction(ξy) and the height(z) was derived.The fraction(ξy) was paralleled with dune surface and vertical with airflow direction.This result demonstrated that airflow particles moved horizontally as well as rotated.That meant airflow particles move just like a cycloidal movement.The mutual overlaps of different scales of waves formed orderly fluctuations;then sand particles are eroded at dune peak and pile up in dune valley,and the dunes formed eventually.

Key words: sand ripple, horizontal vorticity, airflow fluctuation

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