摘要
A vertical phase shift of the diurnal harmonic of geopotential height S1(Z) in the lower troposphere of low latitudes is shown by a comparison of diurnal harmonic of surface pressure at two surface stations that have an elevation difference close to 4 km. It is inferred from longitude-height cross sections of S1(Z) that this vertical phase shift is caused by the differential response of the lower and mid-upper troposphere to the diurnal variation of radiative heating/cooling.
| 原文 | ???core.languages.en_GB??? |
|---|---|
| 頁（從 - 到） | 3793-3797 |
| 頁數 | 5 |
| 期刊 | Journal of Climate |
| 卷 | 14 |
| 發行號 | 17 |
| DOIs | |
| 出版狀態 | 已出版 - 1 9月 2001 |