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Process / pipelineDynamical meteorology

Upepo Joto

Uhusiano wa upepo joto ni kanuni ya msingi ya hali ya hewa inayounganisha mkasi wa upepo wima na miteremko ya halijoto ya mlalo. Inasema kwamba kasi ya upepo huongezeka kadiri urefu unavyoongezeka kuelekea upande wa joto—matokeo ya moja kwa moja ya usawa wa haidrostatiki na kijiostrofiki pamoja na sheria ya gesi bora.

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Vyanzo

  1. Holton, J. R. (2004). An Introduction to Dynamic Meteorology (4th ed.). Academic Press. link
  2. Bluestein, H. B. (1993). Synoptic-dynamic meteorology in midlatitudes. Volume 2: Observations and Theory of Weather Systems. Oxford University Press. link

Jinsi ya kunukuu ukurasa huu

ScholarGate. (2026, June 3). Thermal Wind Relationship. ScholarGate. https://scholargate.app/sw/meteorology/thermal-wind

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Imerejelewa na

ScholarGateThermal Wind (Thermal Wind Relationship). Imepatikana 2026-06-17 kutoka https://scholargate.app/sw/meteorology/thermal-wind · Seti ya data: https://doi.org/10.5281/zenodo.20539026