Категория:Моделирование рельефа: различия между версиями
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* [https://www.sciencedaily.com/releases/2017/01/170130224728.htm The movement of water in the ocean is determined by many factors including tides; winds; surface waves; internal waves, those that propagate within the layers of the ocean; and differences in temperature, salinity or sea level height. Additionally, like high and low pressure systems seen on TV weather maps, the ocean is full of eddies, slowly swirling masses of water... In the future, Qiu and colleagues hope to develop a mathematical approach to creating more detailed pictures of circulation based on sea level in more locations throughout the Pacific.] | * [https://www.sciencedaily.com/releases/2017/01/170130224728.htm The movement of water in the ocean is determined by many factors including tides; winds; surface waves; internal waves, those that propagate within the layers of the ocean; and differences in temperature, salinity or sea level height. Additionally, like high and low pressure systems seen on TV weather maps, the ocean is full of eddies, slowly swirling masses of water... In the future, Qiu and colleagues hope to develop a mathematical approach to creating more detailed pictures of circulation based on sea level in more locations throughout the Pacific.] | ||
* [[:Category:Инерционный калькулятор|Инерционный калькулятор]] | * [[:Category:Инерционный калькулятор|Инерционный калькулятор]] | ||
| − | + | * [[Модель рельефа Земли]] | |
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Версия 16:53, 28 ноября 2018
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- The movement of water in the ocean is determined by many factors including tides; winds; surface waves; internal waves, those that propagate within the layers of the ocean; and differences in temperature, salinity or sea level height. Additionally, like high and low pressure systems seen on TV weather maps, the ocean is full of eddies, slowly swirling masses of water... In the future, Qiu and colleagues hope to develop a mathematical approach to creating more detailed pictures of circulation based on sea level in more locations throughout the Pacific.
- Инерционный калькулятор
- Модель рельефа Земли
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