Abstract This study investigates the relative importance of lower atmospheric versus in situ forcing in driving migrating and nonmigrating diurnal and semidiurnal tides in the thermosphere, as well as the impact of solar and geomagnetic activity on these tides. Our focus is the “thermospheric gap” region 110–250 km, where few observations are available but the tidal spectrum is known to change dramatically. We employ the Hough Mode Extension (HME) fitting approach to the Specified Dynamics Whole Atmosphere Community Climate Model with thermosphere‐ionosphere eXtension (SD‐WACCM‐X) to separate upward‐propagating tides originating from tropospheric and stratospheric sources from those generated in situ within the thermosphere and calculate their ratio to quantify their relative importance. To assess the extent to which the solar and geomagnetic activity impact these thermospheric tides, we compare SD‐WACCM‐X simulations with control simulations in which geomagnetic (Kp) and solar (F10.7) activity are held at lower fixed values. Focusing on the year 2014, a period characterized by elevated solar and geomagnetic variability, we analyze how these external drivers modify tidal amplitudes as a function of latitude and season. The model simulations are validated by comparison with independent neutral density tide observations from the CHAllenging Minisatellite Payload data at approximately 390 km altitude from 2002 to 2004 (F10.7 = 140 sfu). The results highlight the critical role of both thermospheric and lower atmospheric forcings in shaping tidal dynamics, which has implications for forthcoming satellite missions targeting the space weather of the ionosphere‐thermosphere system and improving space operations in the very low Earth orbit.
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This content will become publicly available on March 1, 2027
Thermospheric Energy and Heating Due To Upward Propagating and in Situ Generated Tides During Solar Cycle 24
Abstract We investigate vertical and horizontal energy transport and associated heating in the thermosphere due to both upward propagating and in situ generated migrating and nonmigrating diurnal and semidiurnal tides over the solar cycle 24 (2009–2019). Upward propagating tidal fields are derived from wind and temperature observations from the TIDI and SABER instruments onboard the TIMED satellite, utilizing the Hough Mode Extension (HME) fitting approach. Using these observational tidal fields and fluid dynamic equations, we characterize both vertical and horizontal wave energy fluxes in the 80–250 km altitude range, providing a detailed view of how tidal energy varies throughout the thermosphere. Corresponding thermospheric heating rates are also derived from the observed tidal fields. To assess the contribution of in situ generated thermospheric tides to tidal energy and heat budget, we employ the same approach to the Specified Dynamics Whole Atmosphere Community Climate Model with thermosphere‐ionosphere eXtension (SD‐WACCM‐X) simulations for the same period and find that in situ generated tidal energy flux dominates the upper thermosphere. Our results reveal the temporal evolution of tidal energy fluxes across solar activity levels, as well as the complex interplay between vertical and horizontal energy redistribution, identifying regions of tidal energy sources and sinks. These findings improve our understanding of tidal energy transport in determining the dynamics and energetics in very low Earth orbit, the new frontier of space operations.
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- Award ID(s):
- 2149695
- PAR ID:
- 10680082
- Publisher / Repository:
- AGU Wiley
- Date Published:
- Journal Name:
- Journal of Geophysical Research: Space Physics
- Volume:
- 131
- Issue:
- 3
- ISSN:
- 2169-9380
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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