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Process / pipelineDynamical Oceanography

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.

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Vyanzo

  1. 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
  2. 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

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Imerejelewa na

ScholarGateEkman Transport (Ekman Transport Calculation). Imepatikana 2026-06-15 kutoka https://scholargate.app/sw/oceanography/ekman-transport · Seti ya data: https://doi.org/10.5281/zenodo.20539026