Intensive circulation of bottom waters with higher contents of dissolved oxygen may have caused the formation of the CORBs.
富氧的底层洋流作用导致底层水含氧量增加是红层形成的主要原因。
Intensive circulation of bottom waters with higher contents of dissolved oxygen may have caused the formation of the CORBs.
富氧的底层洋流作用导致底层水含氧量增加是红层形成的主要原因。
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