Usafirishaji wa Ekman
Usafirishaji wa Ekman ni mtiririko wa jumla wa maji unaosababishwa na msukumo wa upepo unaosawazishwa na nguvu ya Coriolis katika safu ya mipaka ya uso. Uliandaliwa na Vagn Walfrid Ekman mwaka 1905 kutoka kanuni kwamba msukumo wa upepo huhamishwa kupitia safu ya maji kwa muundo wa duara, usafirishaji wa Ekman unawajibika kwa upandaji wa pwani na usafirishaji muhimu wa bahari. Nadharia hii inaunganisha ruwaza za upepo wa uso moja kwa moja na mzunguko wa bahari.
Soma mbinu kamili
Ingia kwa akaunti ya bure ili kusoma sehemu hii.
Method map
The neighbourhood of related methods — select a node to explore.
Vyanzo
- Ekman, V. W. (1905). On the influence of the Earth's rotation on ocean currents. Arkiv for Matematik, Astronomi och Fysik, 2(11), 1-52. link ↗
- Cushman-Roisin, B., & Beckers, J.-M. (2011). Introduction to Geophysical Fluid Dynamics: Physical and Numerical Aspects. Academic Press. DOI: 10.1016/b978-0-12-088759-0.00001-8 ↗
Jinsi ya kunukuu ukurasa huu
ScholarGate. (2026, June 3). Ekman Transport Calculation. ScholarGate. https://scholargate.app/sw/oceanography/ekman-transport
Which method?
Set this method beside its closest kin and read them side by side — the library lays the books on the table; the choice is yours.
- Kifaa cha Kurekodi Doppler cha SautiOseanografia↔ compare
- Kasi ya KijiografiaOseanografia↔ compare
- Uchambuzi wa Harmoni ya MawimbiOseanografia↔ compare
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