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Process / pipelineBoundary layer theory

Nadharia ya Kufanana ya Monin-Obukhov

Nadharia ya kufanana ya Monin-Obukhov ni mfumo msingi katika meteorolojia ya safu ya mipaka unaoelezea jinsi kasi ya upepo, joto, na unyevu vinavyotofautiana na kimo karibu na uso. Ilichapishwa mwaka 1954, inaonyesha kuwa wasifu wima uliopimwa kwa kiasi unategemea kigezo kimoja kisicho na vipimo—kigezo cha uthabiti cha Monin-Obukhov—ambacho hupima uwiano kati ya msukumo wa mitambo na mchanganyiko wa nguvu.

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Vyanzo

  1. Monin, A. S., & Obukhov, A. M. (1954). Basic laws of turbulent mixing in the ground layer of the atmosphere. Tr. Akad. Nauk SSSR, 24, 163-187. link
  2. Paulson, C. A. (1970). The mathematical representation of wind speed and temperature profiles in the unstable atmospheric surface layer. Journal of Applied Meteorology, 9(6), 857-861. DOI: 10.1175/1520-0450(1970)009<0857:TMROWS>2.0.CO;2

Jinsi ya kunukuu ukurasa huu

ScholarGate. (2026, June 3). Monin-Obukhov Similarity Theory. ScholarGate. https://scholargate.app/sw/meteorology/monin-obukhov-similarity

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Imerejelewa na

ScholarGateMonin-Obukhov Similarity (Monin-Obukhov Similarity Theory). Imepatikana 2026-06-19 kutoka https://scholargate.app/sw/meteorology/monin-obukhov-similarity · Seti ya data: https://doi.org/10.5281/zenodo.20539026