Non-linear pumping effect in oscillatory diffusive processes and its physical consequences for the World Ocean deep layers and lakes
The physical mechanism of heat transmission in oscillatory processes is described. The effect manifestation in the process of integral heat exchange in the World Ocean deep layers is studied with-in the frame of a simple one-dimensional approach. The sea surface temperature (SST) has long-term oscil...
Збережено в:
| Дата: | 2013 |
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| Автор: | |
| Формат: | Стаття |
| Мова: | English |
| Опубліковано: |
Морський гідрофізичний інститут НАН України
2013
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| Назва видання: | Морской гидрофизический журнал |
| Теми: | |
| Онлайн доступ: | http://dspace.nbuv.gov.ua/handle/123456789/105096 |
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| Назва журналу: | Digital Library of Periodicals of National Academy of Sciences of Ukraine |
| Цитувати: | Non-linear pumping effect in oscillatory diffusive processes and its physical consequences for the World Ocean deep layers and lakes / V.N. Zyryanov // Морской гидрофизический журнал. — 2013. — № 5. — С. 18-35. — Бібліогр.: 23 назв. — англ. |
Репозитарії
Digital Library of Periodicals of National Academy of Sciences of Ukraine| Резюме: | The physical mechanism of heat transmission in oscillatory processes is described. The effect manifestation in the process of integral heat exchange in the World Ocean deep layers is studied with-in the frame of a simple one-dimensional approach. The sea surface temperature (SST) has long-term oscillations with amplitudes greater than the trend in mean-temperature increase. The oscillations of SST lead to nonlinear pumping effect in oscillatory processes; heat is pumped out from or into the deep layers, depending on oscillation amplitudes. With increasing SST oscillation amplitudes, the heat comes out and deep layers are cooled, otherwise, with decreasing amplitudes, the heat spreads into the deep layers. |
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