机译:暴风雨中的大气边界层:高级理论和建模应用
It is common knowledge that basic features of PBLs exhibit a noticeabledependence on the free-flow static stability and baroclinicity. However, theconcern of the traditional theory of neural and stable PBLs was almostwithout exception the barotropic nocturnal PBL, which develops at midlatitudes during a few hours in the night, on the background of a neutral orslightly stable residual layer. The latter separates this type of the PBLfrom the free atmosphere. It is not surprising that the nature of turbulencein such regimes is basically local and does not depend on the properties ofthe free atmosphere.
Alternatively, long-lived neutral (in fact only conditionally neutral) orstable PBLs, which have much more time to grow up, are placed immediatelybelow the stably stratified free flow. Under these conditions, the turbulenttransports of momentum and scalars even in the surface layer - far awayfrom the PBL outer boundary - depend on the free-flowBrunt-Väisälä frequency, N.
Furthermore, integral measures of the long-lived PBLs (their depths and theresistance law functions) depend on N and also on the baroclinic shear, S. Inthe traditional PBL models both non-local parameters N and S were overlooked.One of possible mechanisms responsible for non-local features of thelong-lived PBLs could be the radiation of internal gravity waves (IGW) fromthe PBL upper boundary to the free atmosphere and the IGW-induced transportof the squared fluctuations of velocity and potential temperature.
The free-flow stability plays an especially important role in is theconventionally neutral PBLs (those with the zero potential-temperature fluxat the surface: Fθ=0 at z=0, developed against non-zero staticstability in the free atmosphere: NThe above reasoning obviously calls for a comprehensive revision of thetraditional theory. In a series of papers (quoted below in References) anadvanced theory has been proposed. It includes the following developments.
众所周知,PBL的基本特征表现出对自由流动静态稳定性和斜度的明显依赖。然而,传统的神经和稳定PBL理论的关注点几乎没有例外,即正压型夜间PBL,它在中纬度或略微稳定的残余层背景下,于夜间在数小时内在中纬度地区发育。后者将这种类型的PBL与自由气氛区分开来。毫不奇怪,在这种情况下湍流的性质基本上是局部的,并且不依赖于自由气氛的性质。
或者,长期存在的中性(实际上仅是有条件的中性) )稳定的PBL(有更多的成长时间)被放置在稳定分层的自由流下方。在这些条件下,动量和标量的湍流传输(甚至在远离PBL外边界的表层)也取决于自由流动的Brunt-Väisälä频率, N i>。
此外,长寿命PBL的积分测度(其深度和电阻法函数)取决于 N i>,还取决于斜压剪切力 S i>。在传统的PBL模型中,非局部参数 N i>和 S i>都被忽略了。长寿命PBL的非局部特征可能的机制之一可能是内部辐射从PBL上边界到自由大气的重力波(IGW),以及由IGW引起的速度和势能平方波动的传输。
自由流稳定性起着特别重要的作用其作用是常规的中性PBL(表面上的势能温度通量为零:在 z i> = 0时 F i> θ sub> = 0,在自由大气中的非零静态稳定性: N i 0)。 以上推论显然要求对传统理论进行全面修订。在一系列论文(在下面的参考文献中引用)中,提出了一种先进的理论。它包括以下发展。
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机译:暴风雨中的大气边界层:高级理论和建模应用