ATMOSPHERIC HYDROXYL RESPONSE TO THE PARTIAL SOLAR ECLIPSE OF MAY 30, 1984

被引：11

作者：

BURNETT, CR ^{[1
]}

BURNETT, EB ^{[1
]}

机构：

[1] NOAA,AERON LAB REAL5,BOULDER,CO 80303

来源：

GEOPHYSICAL RESEARCH LETTERS | 1985年 / 12卷 / 05期

关键词：

SOLAR RADIATION;

D O I：

10.1029/GL012i005p00263

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

A large amplitude oscillation in the vertical column abundance of atmospheric OH has been observed in ground-based spectroscopic absorption measurements from Fritz Peak Observatory, Colorado (105 degree W, 40 degree N) during and after the partial solar eclipse of May 30, 1984. An initial OH reduction during the eclipse was followed by an underdamped oscillation having a period of about one hour; the OH abundances returned to normal values two hours after the eclipse termination. This is believed to be the first observation of a 'ringing' response of any atmospheric constituent to a solar eclipse. Refs.

引用

页码：263 / 266

页数：4

共 8 条

[1] MEASUREMENT OF O-2(ALPHA-1-DELTA-G) EMISSION IN A TOTAL SOLAR ECLIPSE [J].