Greg Okin

Prof. Greg Okin

1. Department of Geography, University of California, Los Angeles, CA 90095, USA
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orcid

Research Focus & Metrics

Academic Career Length

32Years (1995-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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31 December 2008 in Global Biogeochemical Cycles
Verified
Journal Article
Open access
PDF file
NMNatalie Mahowald
Natalie Mahowald
TJTimothy D. Jickells
Timothy D. Jickells
ABAlex R. Baker
Alex R. Baker
Paulo ArtaxoPaulo Artaxo
Paulo Artaxo
Claudia Benitez-NelsonClaudia Benitez-Nelson
Claudia Benitez-Nelson
STSeigen Tsukuda
Seigen Tsukuda
A worldwide compilation of atmospheric total phosphorus (TP) and phosphate (PO4) concentration and deposition flux observations are combined with transport model simulations to derive the global distribution of concentrations and deposition fluxes of TP and PO4. Our results suggest that mineral aerosols are the dominant source of TP on a global scale (82%), with primary biogenic particles (12%) and combustion sources (5%) important in nondusty regions. Globally averaged anthropogenic inputs are estimated to be ∼5 and 15% for TP and PO4, respectively, and may contribute as much as 50% to the deposition over the oligotrophic ocean where productivity may be phosphorus‐limited. There is a net loss of TP from many (but not all) land ecosystems and a net gain of TP by the oceans (560 Gg P a−1). More measurements of atmospheric TP and PO4 will assist in reducing uncertainties in our understanding of the role that atmospheric phosphorus may play in global biogeochemistry.

21 April 2004 in Global Biogeochemical Cycles
Verified
Journal Article
Closed access
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GOGreg Okin
Greg Okin
NMNatalie Mahowald
Natalie Mahowald
OCOliver A. Chadwick
Oliver A. Chadwick
Paulo ArtaxoPaulo Artaxo
Paulo Artaxo

20 October 2011 in Ecohydrology
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Journal Article
Closed access
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PDPaolo D'Odorico
Paolo D'Odorico
GOGreg Okin
Greg Okin
BBBrandon T. Bestelmeyer
Brandon T. Bestelmeyer

12 July 2007 in Biogeochemistry
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Journal Article
Closed access
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JLJunran Li
Junran Li
GOGreg Okin
Greg Okin
LALorelei Alvarez
Lorelei Alvarez
HEHoward Epstein
Howard Epstein

3 August 2011 in Reviews of Geophysics
Verified
Journal Article
Closed access
PDF file
SRSujith Ravi
Sujith Ravi
PDPaolo D'Odorico
Paolo D'Odorico
DBDavid D. Breshears
David D. Breshears
JFJason P. Field
Jason P. Field
AGAndrew S. Goudie
Andrew S. Goudie
TZTed M. Zobeck
Ted M. Zobeck

12 October 2009 in Frontiers in Ecology and the Environment
Verified
Journal Article
Open access
PDF file
JFJason P Field
Jason P Field
JBJayne Belnap
Jayne Belnap
DBDavid D Breshears
David D Breshears
JNJason Neff
Jason Neff
GOGreg Okin
Greg Okin
RRRichard L Reynolds
Richard L Reynolds
Wind erosion and associated dust emissions play a fundamental role in many ecological processes and provide important biogeochemical connectivity at scales ranging from individual plants up to the entire globe. Yet, most ecological studies do not explicitly consider dust‐driven processes, perhaps because most relevant research on aeolian (wind‐driven) processes has been presented in a geosciences rather than an ecological context. To bridge this disciplinary gap, we provide a general overview of the ecological importance of dust, examine complex interactions between wind erosion and ecosystem dynamics from the scale of plants and surrounding space to regional and global scales, and highlight specific examples of how disturbance affects these interactions and their consequences. It is likely that changes in climate and intensification of land use will lead to increased dust production from many drylands. To address these issues, environmental scientists, land managers, and policy makers need to consider wind erosion and dust emissions more explicitly in resource management decisions.