Hadley cell

名詞

(meteorology) A global-scale tropical atmospheric circulation that features air rising near the Equator, flowing poleward at a height of 10 to 15 kilometers above the earth's surface, descending in the subtropics, and then returning equatorward near the surface. This circulation creates the trade winds, tropical rain-belts and hurricanes, subtropical deserts and the jet streams.

日本語の意味

ハドレー循環（気象学）: 地球規模の熱帯大気循環で、赤道付近で空気が上昇し、地上約10～15kmの高度で極方向へ流れ、亜熱帯で下降し、その後再び赤道方向に戻る現象。この循環により貿易風、熱帯雨帯、ハリケーン、亜熱帯の砂漠、ジェット気流などが形成される。

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Meteorologists study the Hadley cell to understand why the tropics have intense convection and why deserts form in the subtropics.

気象学者はハドレー循環を研究して、熱帯で激しい対流が起こる理由や亜熱帯で砂漠が形成される理由を解明しようとしている。

詳細

意味（1）

(meteorology) A global-scale tropical atmospheric circulation that features air rising near the Equator, flowing poleward at a height of 10 to 15 kilometers above the earth's surface, descending in the subtropics, and then returning equatorward near the surface. This circulation creates the trade winds, tropical rain-belts and hurricanes, subtropical deserts and the jet streams.

Hadley cells （ plural ）