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    Spatial and Temporal Transferability of a Distributed Energy-Balance Glacier Melt Model 

    Source: Journal of Climate:;2010:;volume( 024 ):;issue: 005:;page 1480
    Author(s): MacDougall, Andrew H.; Flowers, Gwenn E.
    Publisher: American Meteorological Society
    Abstract: Modeling melt from glaciers is crucial to assessing regional hydrology and eustatic sea level rise. The transferability of such models in space and time has been widely assumed but rarely tested. To investigate melt model ...
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    The Origin and Limits of the Near Proportionality between Climate Warming and Cumulative CO2 Emissions 

    Source: Journal of Climate:;2015:;volume( 028 ):;issue: 010:;page 4217
    Author(s): MacDougall, Andrew H.; Friedlingstein, Pierre
    Publisher: American Meteorological Society
    Abstract: he transient climate response to cumulative CO2 emissions (TCRE) is a useful metric of climate warming that directly relates the cause of climate change (cumulative carbon emissions) to the most used index of climate change ...
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    If Anthropogenic CO2 Emissions Cease, Will Atmospheric CO2 Concentration Continue to Increase? 

    Source: Journal of Climate:;2013:;volume( 026 ):;issue: 023:;page 9563
    Author(s): MacDougall, Andrew H.; Eby, Michael; Weaver, Andrew J.
    Publisher: American Meteorological Society
    Abstract: f anthropogenic CO2 emissions were to suddenly cease, the evolution of the atmospheric CO2 concentration would depend on the magnitude and sign of natural carbon sources and sinks. Experiments using Earth system models ...
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    The Uncertainty in the Transient Climate Response to Cumulative CO2 Emissions Arising from the Uncertainty in Physical Climate Parameters 

    Source: Journal of Climate:;2016:;volume( 030 ):;issue: 002:;page 813
    Author(s): MacDougall, Andrew H.; Swart, Neil C.; Knutti, Reto
    Publisher: American Meteorological Society
    Abstract: n emergent property of most Earth system models is a near-linear relationship between cumulative emission of CO2 and change in global near-surface temperature. This relationship, which has been named the transient climate ...
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