Abstract Using polar mesosphere summer echoes and stratospheric/mesospheric winds to explain summer mesopause jumps in Antarctica
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Using polar mesosphere summer echoes and stratospheric/mesospheric winds to explain summer mesopause jumps in Antarctica

机译:使用极性介质夏季回声和平流层/伴游风向解释夏季中间春季在南极洲跳跃

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Abstract Recent high resolution temperature measurements by resonance lidar occasionally showed a sudden mesopause altitude increase by ~5km and an associated mesopause temperature decrease by ~10K at Davis (69°S). In this paper we present further observations which are closely related to this ‘mesopause jump’, namely the increase of mean height of polar mesospheric summer echoes (PMSE) observed by a VHF radar, very strong westward winds in the upper mesosphere measured by an MF radar, and relatively large eastward winds in the stratosphere taken from reanalysis. We present a detailed explanation of mesopause jumps. They occur only when stratospheric winds are moderately eastward and mesospheric winds are strongly westward. Under these conditions, gravity waves with comparatively large eastward phase speeds can pass the stratosphere and propagate to the lower thermosphere because their vertical wavelengths in the mesosphere are rather large which implies enhanced dynamical stability. When finally breaking in the lower thermosphere, these waves drive an enhanced residual circulation that causes a cold and high-altitude mesopause. The conditions for a mesopause jump occur only in the Southern Hemisphere (SH) and are associated with the late breakdown of the polar vortex. Mesopause jumps are primarily, but not only, observed prior and close to solstice. Our study also shows that during the onset of PMSE in the SH, stratospheric zonal winds are still eastward (up to 30m/s), and that the onset is not closely related to the transition of the stratospheric circulation. Unlike previously published results with polar mesospheric clouds, we find an overall poor correlation between PMSE onset and the date of the vortex breakdown. Highlights ? We present new observations from Antarctica (69°S) related to mesopause jumps. ? Mesopause jumps become manifest in a rapid increase of PMSE altitudes. ? Mesopause jumps are explained considering stratospheric/mesopheric circulation. ? Propagation conditions for gravity waves are crucial for mesopause jumps. ? In the SH the onset of PMSE it not a good indicator for winter/summer transition. ? Mesopause jumps are exclusive
机译:<![cdata [ 抽象 最近的高分辨率温度测量突然显示突然的中断高度增加〜5 km在戴维斯(69°S)下,相关的中小期温度降低〜10 k。在本文中,我们提出了与这种“中一体跳跃”密切相关的进一步观察,即由VHF雷达观察到的极地态度夏季回声(PMSE)的平均高度的增加,由MF测量的上部介质层中的上部椎间圈中非常强烈的向西风雷达,以及从重新分析中取得的平流层中的相对大的向东风。我们展示了一个细微的解释跳跃。只有当划分的风时东时,它们只是在向东和Mesospheric风中强烈向西。在这些条件下,具有相对大的东相速度的重力波可以通过平流层并传播到下热层,因为介质层中的垂直波长相当大,这意味着增强的动态稳定性。当最后在较低的热层中破碎时,这些波浪驱动增强的残余循环,导致冷和高海拔中断。跳跃的条件仅在南半球(SH)中发生,并且与极性涡旋的后期分解相关。跳跃主要是,但不仅在透视之前观察到的。我们的研究还表明,在SH中的PMSE发作期间,Stratospheric Zonal Winds仍然向东(最多30 M / s),并且发病并不与之密切相关平流层循环的过渡。与以前公布的彩色态度云出版的结果,我们发现PMSE发作与涡旋故障日期之间的总体相关性差。 突出显示 < CE:PARA ID =“P5015”View =“全部”>我们呈现与南极洲(69°S)相关的新观察与中断跳跃相关的南极(69°S)。 Mesopause跳跃在PMSE海拔快速增加时变得显现。 mesopause跳转是探索考虑到平坦化/脑血管循环。 在sh中的PMSE发作,这不是冬季/夏季过渡的良好指标。 mesopause jumps是独家

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