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The advances and retreats of the Alpine glaciers show a surprising correspondence to the up and declined states of the tree-growths at Arlieshan Mt. (23°30′N 120°48′E 2676M) in Formosa, as shown in Fig. 3. It is supposed that the intensified state of jet stream would result the retreat of glaciers in the Alps, activating the lateral mixings of cold and warm air, while, in the Far East, the stronger jet would repress the amount of summer precipitations of the south-eastern monsoons on which tree-growths might depend. (See Fig. 2)

Relationships of the Secular Change of Jet Stream with the Activities of Glaciers