Thermospheric wind around the cusp

Abstract

The thermosphere is the transition region from the dense atmosphere to space. Winds in the thermosphere affect not only thermospheric mass density, composition, and temperature, but also ionospheric electrodynamics, altering Joule heating and causing wind-driven field-aligned currents. An understanding of winds is needed for space physics research and space weather applications. This project aims to investigate upper thermospheric winds around the cusp, where the solar wind penetrates to the ionosphere in a narrow funnel. We will examine the pattern and forcing of the winds, and the relation of the winds with the thermosphere density anomaly. The project is compelling because the cusp is one of the two main regions of energy input from the magnetosphere, the other being the nightside auroral zone. The energy input comes in the form of Poynting flux and soft particle precipitation. We will conduct the project by coordinating observations from multiple sources and validating and enhancing thermospheric models. Specifically, upper thermospheric winds will be obtained by Scanning Doppler Imagers. Ionospheric plasma convection will be obtained from the Super Dual Auroral Radar Network. Poynting flux flowing into the cusp and neutral density will be estimated using Swarm. The Global Ionosphere Thermosphere Model will be used to examine forcing of winds and the physical relation between winds and neutral density self-consistently.

Document Details

Document Type
DoD Grant Award
Publication Date
Mar 07, 2024
Source ID
FA95502310586

Entities

People

  • Ying Zou

Organizations

  • Air Force Office of Scientific Research
  • Johns Hopkins University
  • United States Air Force

Tags

Fields of Study

  • Environmental science

Readers

  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers
  • Space/Atmospheric Physics.

Technology Areas

  • Space