Abstract
This paper describes a short story of how I learned in early days in space physics (1960–1970) that there are the direct and feed-back relationships between geomagnetic storms and auroral/magnetospheric substorms. In those days, both geomagnetic storms and auroral substorms were almost independent subjects. It is now understood that auroral substorms are directly related to the development of the ring current and thus of the main phase of geomagnetic storms. Further, we have begun to recognize that the growth of the ring current (caused by auroral/magnetospheric substorms) will change the internal structure of the magnetosphere, which in turn will change and could modify at least the intensity of auroral substorms. Thus, there are interesting feed-back processes between them. It is expected that this feed-back relationship between geomagnetic storms and auroral/magnetospheric substorms will become one of the major issues in magnetospheric physics in the future. In fact, an effort to understand this relationship will deepen our understanding of both geomagnetic storms and auroral/magnetospheric substorms. The progress in understanding the relationship between auroral substorms and geomagnetic storms is an example, in which it takes a long time to advance even one step. It is hoped that this paper will serve to learn the background in the development of space physics in the early days.
Highlights
HISTORYIt had been well known from early days that intense geomagnetic storms are associated with great auroral displays
This paper describes a short story of how I learned in early days in space physics (1960–1970) that there are the direct and feed-back relationships between geomagnetic storms and auroral/magnetospheric substorms
I began to study auroral displays and established the present concept of auroral substorms (Akasofu, 1964). It was during the course of a study of auroral substorms, I learned that auroral substorms are directly responsible for the cause of the main phase of geomagnetic storms by the fact that auroral substorms inject protons into the ring current belt (Deforest and McIlwain, 1971)
Summary
It had been well known from early days that intense geomagnetic storms are associated with great auroral displays. Both subjects were treated as almost independently in those days. I began to study auroral displays and established the present concept of auroral substorms (Akasofu, 1964). It was during the course of a study of auroral substorms, I learned that auroral substorms are directly responsible for the cause of the main phase of geomagnetic storms by the fact that auroral substorms inject protons into the ring current belt (Deforest and McIlwain, 1971). One of them was the discovery that ionospheric oxygen atoms (ionized) are the main
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