海洋热梯度
海洋表层与深层间出现随深度增大而逐渐加大的温差，称为海洋热梯度。一般情况下，如热梯度大于18℃时，便有开发利用的价值。尤其是温差达到20℃时，能量稳定，昼夜少明显变化，更居可开发利用的首位。
117
Alias
Contributor
contributed at 2011-12-26
Classification(s)
●
Earth System(in Chinese) Resource and energy geography
Detailed Description
| English |
|---|
| Name | ocean thermal gradient |
| Chinese |
|---|
| Name | 海洋热梯度 |
| Description | 海洋表层与深层间出现随深度增大而逐渐加大的温差，称为海洋热梯度。一般情况下，如热梯度大于18℃时，便有开发利用的价值。尤其是温差达到20℃时，能量稳定，昼夜少明显变化，更居可开发利用的首位。 |
How to Cite
NNU_Group (2011). 海洋热梯度, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/2b598a9a-b80b-4f27-851b-134216d5dceb
Copy
Copyright and Disclaimer
All copyrights of a material (model, data, article, etc.) in the OpenGMS fully belong to its author/developer/designer (or any other wording about the owner). The OpenGMS takes every care to avoid copyright infringement, contributor(s) should carefully employ materials from other sources and give proper citations.
