stratopause
英：['streɪtəpɔ:z] 美： ['streɪtəˌpɔz]
stratopause 基本解释
n.平流层顶；
英英释义
Stratopause
The stratopause (formerly Mesopeak) is the almost center of the atmosphere which is the numeric between two layers, stratosphere and the mesosphere. In the stratosphere the temperature increases with altitude, and the stratopause is the section where a maximum in the temperature occurs.以上来源于:Wikipedia
stratopause 相关例句
权威例句
Instability at the Winter Stratopause: A Mechanism for the 4-Day Wave.Dynamical response to the solar cycle: Winter stratopause and lower stratosphereEvidence for High-Frequency Synoptic Disturbances Near the Stratopause.The temperature dependence of the ozone concentration near the stratopauseInteraction of the quasi‐biennial oscillation and stratopause semiannual oscillationThe evolution of the stratopause during the 2006 major warming: Satellite data and assimilated meteorological analysesA note on record‐high temperatures at the northern polar stratopause in winter 1997/98Water vapor, molecular hydrogen, methane, and tritium concentrations near the stratopauseConsistent Simulation of Bromine Chemistry From the Marine Boundary Layer to the StratopauseLidar Observations of Gravity Waves and Their Spectra near the Mesopause and Stratopause at Arecibo.
