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    Precessional Cycles and Their Influence on the North Pacific and North Atlantic Summer Anticyclones 

    Source: Journal of Climate:;2013:;volume( 026 ):;issue: 013:;page 4596
    Author(s): Mantsis, Damianos F.; Clement, Amy C.; Kirtman, Ben; Broccoli, Anthony J.; Erb, Michael P.
    Publisher: American Meteorological Society
    Abstract: he response of the Northern Hemisphere summer anticyclones to a change in the timing of perihelion is investigated using the GFDL Climate Model version 2.1 (CM2.1). The orbital forcing consists of changes in the seasonal ...
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    Mechanisms of Mid-Holocene Precipitation Change in the South Pacific Convergence Zone 

    Source: Journal of Climate:;2013:;volume( 026 ):;issue: 018:;page 6937
    Author(s): Mantsis, Damianos F.; Lintner, Benjamin R.; Broccoli, Anthony J.; Khodri, Myriam
    Publisher: American Meteorological Society
    Abstract: he variability of the South Pacific convergence zone (SPCZ) during the mid-Holocene is investigated using models archived in the Paleoclimate Modelling Intercomparison Project Phase II (PMIP2) database. Relative to ...
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    Climate Feedbacks in Response to Changes in Obliquity 

    Source: Journal of Climate:;2011:;volume( 024 ):;issue: 011:;page 2830
    Author(s): Mantsis, Damianos F.; Clement, Amy C.; Broccoli, Anthony J.; Erb, Michael P.
    Publisher: American Meteorological Society
    Abstract: he feedbacks involved in the response of climate to a reduction of Earth?s obliquity are investigated in the GFDL Climate Model version 2.1 (CM2.1). A reduction in obliquity increases the meridional gradient of the annual ...
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    The Response of Large-Scale Circulation to Obliquity-Induced Changes in Meridional Heating Gradients 

    Source: Journal of Climate:;2014:;volume( 027 ):;issue: 014:;page 5504
    Author(s): Mantsis, Damianos F.; Lintner, Benjamin R.; Broccoli, Anthony J.; Erb, Michael P.; Clement, Amy C.; Park, Hyo-Seok
    Publisher: American Meteorological Society
    Abstract: he inter- and intrahemispheric climate responses to a change in obliquity are investigated using the Geophysical Fluid Dynamics Laboratory Climate Model, version 2.1. (GFDL CM2.1). Reduced obliquity causes a weakening of ...
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