Quick Search:       Advanced Search
DIAO HUANXIANG. 1986. MECHANISM STUDY OF MINIMUM VALUE OF DISSOLVED OXYGEN IN ITS VERTICAL DISTRIBUTION IN THE PACIFIC OCEAN. Acta Oceanologica Sinica, (4):537-542
MECHANISM STUDY OF MINIMUM VALUE OF DISSOLVED OXYGEN IN ITS VERTICAL DISTRIBUTION IN THE PACIFIC OCEAN
MECHANISM STUDY OF MINIMUM VALUE OF DISSOLVED OXYGEN IN ITS VERTICAL DISTRIBUTION IN THE PACIFIC OCEAN
Received:February 20, 1985  Revised:February 02, 1986
DOI:
Key words:
中文关键词:  
基金项目:
Author NameAffiliation
DIAO HUANXIANG Institute of Oceanology, Academia Sinica, Qingdao 
Hits: 688
Download times: 593
Abstract:
      The formative mechanism of the minimum value of dissolved oxygen in its vertical distribution in the Pacific Ocean is systematically discussed according to distributive characteristics of oxygen and relative parameters. The t and σt thermoclines of certain intensity controlled by water temperature is an elemental cause of forming minimum value of dissolved oxygen in the Pacific Ocean, whose genesis model of minimum value is presented by the author.
中文摘要:
      The formative mechanism of the minimum value of dissolved oxygen in its vertical distribution in the Pacific Ocean is systematically discussed according to distributive characteristics of oxygen and relative parameters. The t and σt thermoclines of certain intensity controlled by water temperature is an elemental cause of forming minimum value of dissolved oxygen in the Pacific Ocean, whose genesis model of minimum value is presented by the author.
HTML View Full Text   View/Add Comment  Download reader
Close