Éfék Coriolis

Dina fisika, éfék Coriolis nyaéta méngkolna arah barang anu usik nalika ditempo ti carangka acuan anu muter. Barang anu usik lempeng dina carangka muter, baris kasampak méngkol ku pengamat anu cicing dina carangka éta. (tempo gambar)

Éfék ieu bisa ditembrakkeun maké eksperimen sapertos bandul Foucault. Carana nyaéta ngagantungkeun hiji bandul sarta diayunkan sacara terus-terusan, éta bandul gerakna moal ka arah nu sarua terus, tapi bakal ngagésér ka arah anu séjén.

Di Bumi, éfék Coriolis bisa dirasakeun dina pergerakan dina jarak anu laér sarta période anu panjang, misalna pergerakan hawa anu skalana badag di atmosfer atawa cai di samudra.

Istilah ieu dicokot tina ngaran ilmuwan Perancis Gaspard-Gustave Coriolis (1792).

Tumbu luar 

 The definition of the Coriolis effect from the Glossary of Meteorology

 The Coriolis Effect PDF-file. 17 pages. A general discussion by Anders Persson of various aspects of the coriolis effect, including Foucault's Pendulum and Taylor columns.
 Anders Persson The Coriolis Effect: Four centuries of conflict between common sense and mathematics, Part I: A history to 1885 History of Metéorology 2 (2005)
 10 Coriolis Effect Videos and Games- from the About.com Wéather Page
 Coriolis Force - from ScienceWorld
 Coriolis Effect and Drains An article from the NEWTON web site hosted by the Argonne National Laboratory.

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