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David J. Erickson
Researcher at Oak Ridge National Laboratory
Publications - 82
Citations - 8958
David J. Erickson is an academic researcher from Oak Ridge National Laboratory. The author has contributed to research in topics: Climate model & Climate change. The author has an hindex of 38, co-authored 82 publications receiving 8377 citations. Previous affiliations of David J. Erickson include National Center for Atmospheric Research & Goddard Space Flight Center.
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Responses of energy use to climate change: A climate modeling study
TL;DR: In this article, the authors show that the high-DT scenario had significantlyincreased warming, especially in winter, so decreased heating needs led to a cumulative (2003-2025) heating/cooling energy decrease of 0.82 quads.
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Effects of solar UV radiation and climate change on biogeochemical cycling: interactions and feedbacks
TL;DR: It is clear that the future changes in UV radiation coupled with human-caused global change will have large impacts on biogeochemical cycles at local, regional and global scales.
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Interactive effects of ozone depletion and climate change on biogeochemical cycles
TL;DR: The effects of ozone depletion on global biogeochemical cycles, via increased UV-B radiation at the Earth's surface, have continued to be documented over the past 4 years.
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On the global flux of atmospheric sea salt
David J. Erickson,Robert A. Duce +1 more
TL;DR: In this article, the global wet and dry deposition fields of atmospheric sea salt to the ocean surface, obtained using a sea-salt mass size distribution appropriate for an elevation of 15 m above mean sea level (AMSL), are examined on a monthly basis with 5° × 5° latitude-longitude spatial resolution.
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Quantifying the effects of CO2‐fertilized vegetation on future global climate and carbon dynamics
S. L. Thompson,B. Govindasamy,Art Mirin,Ken Caldeira,Christine Delire,Christine Delire,Jose Milovich,M. Wickett,David J. Erickson +8 more
TL;DR: In this paper, the authors evaluate the approximate upper and lower limits of land carbon uptake using a comprehensive climate-carbon model and show that current uncertainties preclude determination of whether the land biosphere will amplify or damp atmospheric CO{sup 2} increases by the end of the century.