The release of TIEGCM 3.0 in 2024 is a joint effort from researchers worldwide over the past decade. It improves the thermosphere-ionosphere simulation by  introducing new physics or correcting existing deficiencies. However, three major weaknesses still exist and remain to be addressed: Electrodynamics, pole singularity, and ion density solver. The existing TIEGCM electrodynamics solver finds difficulty in resolving the mesoscale currents as well as the penetration electric field. The finite difference scheme is introducing large discretization error near the pole and causing numerical instabilities. The quasi-static ion velocity and temperature approximation becomes increasingly invalid during big storms and high altitudes. In this presentation, I will talk about the effort that have been made to resolve these three issues.