Haize katabatiko
Haize katabatikoa maldan beherako haizea da, maldaren gainean dagoen aireak horizontalki distantzia batera dagoenak baino dentsitate handiagoa izatearen ondorioz sortzen dena. Haize katabatikoa malda asko hozteagatik sortzen da.[1] Haize hauek, bereziki eskualde handietan eragina dutenean, udazkeneko haizeak deitzen dira. 100 km/h-ko abiadura har dezakete eta hotzak eta beroak izan daitezke.
Erreferentziak
- ↑ Euskalterm: [Hiztegi terminologikoa] [2017]
Kanpo estekak
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Datuak: Q212903
Multimedia: Katabatic wind / Q212903
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Artikulu hau meteorologiari buruzko zirriborroa da. Wikipedia lagun dezakezu edukia osatuz. |
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