2018-2019 USAP Field Season
Troposphere-ionosphere coupling via atmospheric gravity waves
Dr. Vadym V Paznukhov
Supporting Stations: Palmer Station
In the Earth's layered atmosphere, gravity (or internal) waves are quasi-periodic disturbances most familiar as the wave-like cloud patterns observed in the lee of mountain ranges. This project investigates the role of atmospheric gravity waves in the ionosphere-troposphere coupling. Researchers will investigate the dynamics of plasma density irregularities in the ionospheric F-region, and the connection of these irregularities with atmospheric gravity waves. Antarctica is ideally suited to this study as large numbers of gravity waves are observable there and the electromagnetic background is quiet, which is important for detection of the radio signals to be observed in this study.
Field Season Overview
This is the final season of this project. A support contractor research associate will assist in taking down and packing and shipping the equipment and instruments back to the researcher's home institution. Contractor science construction personnel will remove the three antennas in the Palmer Station “backyard.”