The invention relates to the technical field of hydrological
simulation, and particularly discloses an extra-small
watershed layered three-dimensional hydrological-hydrodynamic full-
coupling simulation method, which comprises the following steps: collecting multi-
source data to construct a three-dimensional space discrete grid and dividing initial time units; the
control equation set is converted into an algebraic
system based on a Legendre polynomial and a
Gaussian-Loabar node; adaptively adjusting a time unit length and a spectral
basis function order according to the local time gradient change rate; a convergence
spectral coefficient is obtained through spectral
delay correction iteration solution; and finally, forcibly executing
mass conservation constraint, controlling step recalculation according to a local
time error, and gradually outputting a flow
hydrograph and
water depth and infiltration rate distribution according to time unit endpoints. According to the method, the dual self-adaption of the
time step length and the polynomial order is realized, the numerical oscillation of the infiltration rate caused by the sudden change of the
ponding depth can be effectively inhibited, the
mass conservation is ensured, and the stability and the efficiency of the rainstorm flood
simulation of the extra-small
watershed are improved.