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中国廊坊中间层和低热层大气平均风观测模拟

杨钧烽 肖存英 胡雄 徐轻尘

杨钧烽, 肖存英, 胡雄, 徐轻尘. 中国廊坊中间层和低热层大气平均风观测模拟[J]. 空间科学学报, 2017, 37(3): 284-290. doi: 10.11728/cjss2017.03.284
引用本文: 杨钧烽, 肖存英, 胡雄, 徐轻尘. 中国廊坊中间层和低热层大气平均风观测模拟[J]. 空间科学学报, 2017, 37(3): 284-290. doi: 10.11728/cjss2017.03.284
YANG Junfeng, XIAO Cunying, HU Xiong, XU Qingchen. Observations and Simulations of the Mean Winds in Mesosphere and Lower Thermosphere over Langfang of China[J]. Journal of Space Science, 2017, 37(3): 284-290. doi: 10.11728/cjss2017.03.284
Citation: YANG Junfeng, XIAO Cunying, HU Xiong, XU Qingchen. Observations and Simulations of the Mean Winds in Mesosphere and Lower Thermosphere over Langfang of China[J]. Journal of Space Science, 2017, 37(3): 284-290. doi: 10.11728/cjss2017.03.284

中国廊坊中间层和低热层大气平均风观测模拟

doi: 10.11728/cjss2017.03.284
基金项目: 

国家重点研发计划项目(2016YFB0501503)和国家自然科学基金项目(41104099)共同资助

详细信息
    作者简介:

    肖存英,xiaocy@nssc.ac.cn

  • 中图分类号: P41

Observations and Simulations of the Mean Winds in Mesosphere and Lower Thermosphere over Langfang of China

  • 摘要: 利用中国廊坊站(39.4°N,116.7°E)流星雷达在2012年4月1日至2013年3月31日的水平风场观测数据,分析廊坊上空80~100km的中间层与低热层(Mesosphere and Lower Thermosphere,MLT)大气平均纬向风和经向风的季节变化特征.结果表明平均纬向风和经向风都表现出明显的季节变化特征.平均纬向风在冬季MLT盛行西风,极大值位于中间层顶,随高度增加西风减弱;在夏季中间层为东风,低热层为强西风,风向转换高度约为82km.平均经向风在冬季以南风为主,在夏季盛行北风.纬向风和经向风在春秋两季主要表现为过渡阶段.流星雷达观测结果与WACCM4模式和HWM93模式模拟的气候变化特点基本一致,但WACCM4模式纬向风和经向风风速偏大,而HWM93模式纬向风和经向风风速偏小.

     

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出版历程
  • 收稿日期:  2016-01-25
  • 修回日期:  2016-12-05
  • 刊出日期:  2017-05-15

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