D
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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Journal ArticleDOI
Potential Feedbacks Between Pacific Ocean Ecosystems and Interdecadal Climate Variations
Arthur J. Miller,Michael A. Alexander,George J. Boer,Fei Chai,Kenneth L. Denman,David J. Erickson,Robert Frouin,Albert Jerome Gabric,Edward A. Laws,Marlon R. Lewis,Zhengyu Liu,Ragu Murtugudde,Shoichiro Nakamoto,Douglas J. Neilson,Joel R. Norris,J. Carter Ohlmann,R. Ian Perry,Niklas Schneider,Karen M. Shell,Axel Timmermann +19 more
TL;DR: In this article, oceanic ecosystems altered by interdecadal climate variability may provide a feedback to the physical climate by phytoplankton affecting heat fluxes into the upper ocean anddimethylsulfide fluxes in the atmosphere.
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Effects of stratospheric ozone depletion, solar UV radiation, and climate change on biogeochemical cycling: interactions and feedbacks
TL;DR: The interactive effects of solar UV radiation and climate change on the biogeochemical cycling of aerosols and trace gases other than CO2, as well as of chemical and biological contaminants are assessed.
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Using Clustered Climate Regimes to Analyze and Compare Predictions from Fully Coupled General Circulation Models
TL;DR: In this article, a quantitative statistical clustering technique called Multivariate Spatio-Temporal Clustering (MSTC) was applied to the monthly time series output from a fully coupled general circulation model (GCM) called the Parallel Climate Model (PCM).
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Collapse of the Maya: Could deforestation have contributed?
TL;DR: In this paper, the authors used simulations with a regional climate model to demonstrate that deforestation by the Maya also likely induced warmer, drier, drought-like conditions, and that the combination created a situation the Maya could not recover from.
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Modeling the biogeochemical cycle of dimethylsulfide in the upper ocean: a review
TL;DR: A review of the current DMS modeling approaches, outline the parameterization of key processes, and identify areas where our knowledge is poor and improvements should be made is provided in this article.