The impacts of CO2 radiative forcing versus ocean warming on the Hadley circulation and the ITCZ. (IMAGE)

Science China Press

The impacts of CO2 radiative forcing versus ocean warming on the Hadley circulation and the ITCZ.

Caption

Researchers focus on changes in (A) Southern and (B) northern Hadley cell extent (LatSHC and LatNHC), (C) ITCZ position (LatITCZ), and (D) Northern Hadley cell intensity (IntensityNHC; units, 1010kg∙s-1) during boreal winter (December-January-February, DJF).

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