Michael Ryan

Dr. Michael Ryan


Research Focus & Metrics

Academic Career Length

41Years (1986-Present)

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

Representative Publications

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9 July 2011 in Global Change Biology
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RCRichard T. Conant
Richard T. Conant
MRMichael Ryan
Michael Ryan
GÅGöran I. Ågren
Göran I. Ågren
HHannah Birge
Hannah Birge
EDEric A. Davidson
Eric A. Davidson
MBMark A. Bradford
Mark A. Bradford

17 November 2006 in Ecosystems
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FIF Stuart Chapin Iii
F Stuart Chapin Iii
GWG. M. Woodwell
G. M. Woodwell
JRJ. T. Randerson
J. T. Randerson
ERE. B. Rastetter
E. B. Rastetter
GLG. M. Lovett
G. M. Lovett
ESE.-D. Schulze
E.-D. Schulze
Recent projections of climatic change have focused a great deal of scientific and public attention on patterns of carbon (C) cycling as well as its controls, particularly the factors that determine whether an ecosystem is a net source or sink of atmospheric carbon dioxide (CO2). Net ecosystem production (NEP), a central concept in C-cycling research, has been used by scientists to represent two different concepts. We propose that NEP be restricted to just one of its two original definitions—the imbalance between gross primary production (GPP) and ecosystem respiration (ER). We further propose that a new term—net ecosystem carbon balance (NECB)—be applied to the net rate of C accumulation in (or loss from [negative sign]) ecosystems. Net ecosystem carbon balance differs from NEP when C fluxes other than C fixation and respiration occur, or when inorganic C enters or leaves in dissolved form. These fluxes include the leaching loss or lateral transfer of C from the ecosystem; the emission of volatile organic C, methane, and carbon monoxide; and the release of soot and CO2 from fire. Carbon fluxes in addition to NEP are particularly important determinants of NECB over long time scales. However, even over short time scales, they are important in ecosystems such as streams, estuaries, wetlands, and cities. Recent technological advances have led to a diversity of approaches to the measurement of C fluxes at different temporal and spatial scales. These approaches frequently capture different components of NEP or NECB and can therefore be compared across scales only by carefully specifying the fluxes included in the measurements. By explicitly identifying the fluxes that comprise NECB and other components of the C cycle, such as net ecosystem exchange (NEE) and net biome production (NBP), we can provide a less ambiguous framework for understanding and communicating recent changes in the global C cycle.

7 August 2017 in Nature Ecology & Evolution
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HAHenry Adams
Henry Adams
MZMelanie J. B. Zeppel
Melanie J. B. Zeppel
WAWilliam R. L. Anderegg
William R. L. Anderegg
HHHenrik Hartmann
Henrik Hartmann
SLSimon M. Landhäusser
Simon M. Landhäusser
NMNate G. McDowell
Nate G. McDowell

1 April 1997 in BioScience
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MRMichael Ryan
Michael Ryan
BYBarbara J. Yoder
Barbara J. Yoder
Michael G. Ryan, Barbara J. Yoder; Hydraulic Limits to Tree Height and Tree Growth, BioScience, Volume 47, Issue 4, 1 April 1997, Pages 235–242, https://doi.or

22 July 2007 in Global Change Biology
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CLCreighton M. Litton
Creighton M. Litton
JRJames W. Raich
James W. Raich
MRMichael Ryan
Michael Ryan