Global measurements show that the mixing ratio of tropospheric methane (CH 4 ) increased by 1.1% (19.5 ± 1.7 ppbv) over the five‐year period 1996–2000, with striking fluctuations in its annual growth rate. Whereas the global CH 4 growth rate reached 15.9 ± 0.7 ppbv yr −1 in 1998, the growth rate was −2.1 ± 0.8 ppbv yr −1 in 2000. This is the first time in our 23‐year global monitoring program that we have measured a negative annual CH 4 growth rate. The CH 4 growth rate fluctuates in an unpredictable fashion, and we reemphasize that global CH 4 concentrations cannot be extrapolated into the future based on past trends. As a result, we suggest that the slowing of the CH 4 growth rate during much of the 1980s and 1990s cannot be used to imply that CH 4 will no longer be of concern in greenhouse gas studies during this century.
Ariane Arias‐Ortiz, J. L. Wolfe, Scott D. Bridgham, Sara Knox, Gavin McNicol, Brian A. Needelman, Julie Shahan, Ellen Stuart‐Haëntjens, Lisamarie Windham‐Myers, Patricia Y. Oikawa, Dennis Baldocchi, Joshua S. Caplan, Margaret Capooci, Kenneth M. Czapla, R. Kyle Derby, Heida L. Diefenderfer, Inke Forbrich, Gina N. Groseclose, Jason K. Keller, Cheryl A. Kelley, Amr E. Keshta, Helena S. Kleiner, Ken W. Krauss, Robert R. Lane, Sarah K. Mack, Serena Moseman‐Valtierra, Thomas J. Mozdzer, Peter Mueller, Scott C. Neubauer, Genevieve L. Noyce, Karina V. R. Schäfer, Rebecca Sanders‐DeMott,
Frank E. Anderson, Brian A. Bergamaschi, Cove Sturtevant, Sara Knox, Lauren Hastings, Lisamarie Windham‐Myers, Matteo Detto, Erin L. Hestir, Judith Z. Drexler, Robin L. Miller, Jaclyn Hatala Matthes, Joseph Verfaillie, Dennis Baldocchi, Richard L. Snyder, Roger Fujii
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