The Transfer of Solar Wind Energy to the Venusian Ionosphere Through Magnetic Pumping: Evidence From Pioneer Venus Orbiter Observations

被引:0
|
作者
Fowler, C. M. [1 ]
Frost, A. [2 ]
Agapitov, O. [3 ]
Frahm, R. [4 ]
Xu, S. [3 ]
机构
[1] West Virginia Univ, Dept Phys & Astron, Morgantown, WV 26506 USA
[2] Clarkson Univ, Dept Phys, Potsdam, NY USA
[3] Univ Calif Berkeley, Space Sci Lab, Berkeley, CA USA
[4] Southwest Res Inst, San Antonio, TX USA
关键词
magnetic pumping; Venus; solar wind coupling; ionosphere; plasma heating; Pioneer Venus Orbiter; WHISTLER-MODE WAVES; FLUX ROPES; FIELDS; LIMIT; MARS;
D O I
10.1029/2023GL107756
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The collisionless nature of planetary magnetospheres means that electromagnetic forces are fundamental in controlling the flow of energy and momentum through these systems. We use Pioneer Venus Orbiter (PVO) observations to demonstrate that the magnetic pumping process can be active at Venus, in analogy to its recent discovery at Mars. The presented case study demonstrates the framework for how the process can work at Venus, and the results of a statistical analysis show that the ambient plasma conditions support the process being active. Magnetic pumping enables low frequency magnetosonic waves to heat ambient ionospheric electrons and provides a mechanism that couples the solar wind to the Venusian ionosphere. This is the first time the magnetic pumping process has been discussed at Venus. Our Sun emits a stream of particles outward into our solar system, known as the solar wind. When these particles encounter planets and other bodies (such as comets), they either collide with the body (as happens with our Moon) or are deflected around the obstacle, similar to how water in a stream flows around a rock (this happens at most planets, including Earth, Venus and Mars). Understanding the physical forces that control this deflection enable us to understand how the Sun interacts with the planets in our solar system. We use in situ measurements made by the Pioneer Venus Orbiter spacecraft, which orbited the planet Venus, to investigate one specific process, known as "magnetic pumping." This process allows energy from the solar wind to flow into the Venusian atmosphere. We provide a case study demonstrating how this process can operate at Venus, and show that the average conditions in the near Venus space environment can support this process in a more general sense. A case study demonstrates how the magnetic pumping process operates at Venus Statistical analysis of the plasma conditions at Venus support the notion that magnetic pumping can operate there Magnetic pumping provides an avenue for the solar wind to couple to the Venusian ionosphere and heat ionospheric electrons
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页数:12
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