Numerical modeling of the large-scale neutral and plasma responses to the body forces created by the dissipation of gravity waves from 6 h of deep convection in Brazil

They also excite secondary GWs; those resolved by our global model have λH∼4000–5000 km and cH∼500–600 m/s. These secondary GWs propagate globally and have ƿ√p ~10 – 25% and 5–15% at z=250 and 375 km, respectively. These forces also create plasma perturbations of foF2′∼0.2–1.0 MHz, TEC′∼0.4– 1.5 TECU (total electron content unit, 1TECU  =10¹⁶ elm⁻²), and hmF2′∼5–50 km.

The large-scale traveling ionospheric disturbances (LSTIDs) induced by the secondary GWs have amplitudes of foF2′∼0.2–0.5 MHz, TEC′∼0.2– 0.6 TECU, and hmF2′∼5–10 km. In a companion paper, we discuss changes to the prereversal enhancement and plasma drift from these forces.