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Intertropical convergence zone ITCZ

INDOEX IPCC ITCZ Indian Ocean Experiment Intergovernmental Panel on Climate Change Intertropical Convergence Zone... [Pg.189]

Northern Hemisphere summer insolation during the early to mid-Holocene (Berger, 1978) resulted in increased heating over the Northern Hemisphere continents and thus intensified the thermal contrast between the land and the ocean. The increased heating over the continents resulted in the northward displacement of the intertropical convergence zone (ITCZ) and hence of the monsoon front, while the enhanced land-sea contrast increased the flux of moisture from the ocean to the continent. [Pg.75]

See other pages where Intertropical convergence zone ITCZ is mentioned: [Pg.90]    [Pg.184]    [Pg.271]    [Pg.90]    [Pg.184]    [Pg.271]    [Pg.140]    [Pg.660]    [Pg.39]    [Pg.281]    [Pg.637]    [Pg.222]    [Pg.140]    [Pg.159]    [Pg.983]    [Pg.161]    [Pg.72]    [Pg.99]    [Pg.176]    [Pg.198]    [Pg.876]   


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Convergence zone, intertropical

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