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Local and Remote Responses to Excessive Snow Mass over Eurasia Appearing in the Northern Spring and Summer Climate
Journal of the Meteorological Society of Japan
The effect of excessive snow mass over the Eurasian continent on the spring and summer climate is investigated by using the MRI * GCM. The ensemble mean of the four runs (SNOW runs) with the excessive snow mass of 5 cm (water equivalent) at the beginning of March over the snow cover area of the continent is compared with that of the control runs, to deduce the effect of the snow mass on the climatic parameters in the later seasons. The main results are summarized as follows: (1) In spring, thedoi:10.2151/jmsj1965.69.4_473 fatcat:ekxcem2vdrgdbkuyodxgbe5dlm