A kind of multi-
modal quantitative inversion method of paleoatmospheric circulation based on spatiotemporal
deep learning network, using the powerful non-euclidean space
feature extraction capability of spatiotemporal graph neural network (ST-GNN), captures the nonlinear spatiotemporal
lag effect of
vegetation response to climate; At the same time,
coupling empirical orthogonal function
decomposition (EOF) technology, orthogonal mode is extracted in potential feature space to capture the macroscopic atmospheric teleconnection pattern in geological
record. The present application provides a quantitative inversion paradigm that can integrate micro-ecological mechanism and
macro-dynamic mode, solves the problem of mixed signals in paleoclimate records of Qinghai-Tibet
Plateau and surrounding transition zone, and realizes high-precision and high-resolution restoration of the evolution process of paleoatmospheric circulation intensity. In the multi-source stratigraphic
record verification, not only can the mixed signals be effectively separated, but also the superior robustness and generalization ability are shown when dealing with geological age error and
data loss.