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2 values, were estimated in gyre areas by linear interpolation in both latitude and longitude. In the equatorial zone, where currents are dominated by zonal flows, the value interpolated along the same latitude was used.
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H. Lieth and R. Whittaker, Eds. Ecolog. Stud. 14, Springer, New York
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H. Lieth, in Primary Productivity of the Biosphere, H. Lieth and R. Whittaker, Eds. (Ecolog. Stud. 14, Springer, New York, 1975), pp 203-213.
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(1975)
Primary Productivity of the Biosphere
, pp. 203-213
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Lieth, H.1
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65
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85069284641
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personal communication
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P. Logan, personal communication.
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Logan, P.1
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66
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85069278321
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note
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We thank T. Conway, K. Masarie, K. Thoning, and L. Waterman for obtaining the atmospheric data of the NOAA/GMCC flask network, and many people at the field sites for collecting the air samples over the years. J. John executed 3-D model runs and, together with J. Jonas and P. Palmer, provided support for the color graphics. Assistance by D. Chipman, J. Goddard, S. Sutherland, and E. A. Takahashi is appreciated. R. Gammon and E. Garvey contributed their data to this study. This work has been supported by the Geophysical Monitoring for Climatic Change division of NOAA, the National Science Foundation, Martin Marietta's Carbon Dioxide Information Analysis and Research program for the U.S. Department of Energy under contract DE-AC05-84OR21400, and the EXXON Research and Engineering Company.
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