The Asia monsoon exhibited a decreasing trend ( Figure 9 (b) ) [62] , [63] , as did summer insolation, although winter insolation presented an increasing trend at 25°N ( Figure 9 (c) ) [64] .
← all excerpts
Influence of land development on Holocene Porites coral calcification at Nagura Bay, Ishigaki Island, Japan.
1
—
—