The Production of Temporal Variability in Trace Constituent Concentrations

The Production of Temporal Variability in Trace Constituent Concentrations
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痕量成分浓度随时间变化的产生

DOI:
10.1007/978-94-009-3973-8_20
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发表时间:
1987
影响因子:
6.5
通讯作者:
J. Holton
J. Holton
中科院分区:
物理与天体物理2区
文献类型:
--
作者:
J. Holton

文献摘要

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生产的示踪剂变化的惯性重力波的对比,由于准地转运动。平流层下部臭氧的高频变化往往与潜在温度的波动高度相关,可以解释为惯性重力波导致物质表面垂直位移的证据。从最近的飞机测量的例子。
The production of tracer variability by inertia-gravity waves is contrasted with that due to quasi-geostrophic motions. High frequency variability in ozone in the lower stratosphere is often highly correlated with fluctuations in potential temperature, and can be interpreted as evidence for vertical displacements of material surfaces by inertia gravity waves. Examples are shown from recent aircraft measurements.