We propose a modified spin-wave theory to study the 1/3 magnetization plateau of the antiferromagnetic Heisenberg model on the kagome lattice. By the self-consistent inclusion of quantum corrections, the 1/3 plateau is stabilized over a broad range of magnetic fields for all spin quantum numbers, S. The values of the critical magnetic fields and the widths of the magnetization plateaus are fully consistent with recent numerical results from exact diagonalization and infinite projected entangled paired states. The investigation of low-dimensional frustrated magnetism has become one of the most active frontiers in condensed matter physics. Current frontiers in the field include obtaining full insight into the entanglement structure of quantum many-body wavefunctions for different types of quantum spin liquid [1] and simplex-solid state [2]. Among the many different frustrated systems, quantum antiferromagnets on the kagome lattice are perhaps the most intriguing, because the combination of strong geometric frustration and weak constraints maximizes quantum fluctuation effects. The kagome antiferromagnet has attracted ever-increasing attention over the last two decades, with many different methods applied and resulting proposals for the nature of the ground state [3][4][5][6] One of the characteristic features of kagome antiferromagnets is the appearance of magnetization plateaus in the presence of an external magnetic field. Irrespective of the method applied and the prediction for the zero-field ground state, all theoretical approaches agree that there exists a robust magnetization plateau at m = 1/3 for all values of the spin quantum number, S. The 1/3 plateau has been investigated theoretically by real-space perturbation theory (RSPT) [14], exact diagonalization (ED) [15,16], density-matrix renormalization-group methods (DMRG) [17], and infinite projected entangled paired states (iPEPS) [18]. RSPT provides analytical results for the critical magnetic fields and the width of the plateau [14]. However, a qualitative discrepancy has arisen with recent numerical results from ED [15] and iPEPS [18], not least in that the calculated plateau width increases a 1 a 2