Broecker et al. 1990
Broecker, W.S., T.-H. Peng, J. Jouzel, and G. Russell, 1990: The magnitude of global fresh-water transports of importance to ocean circulation. Clim. Dynam., 4, 73-79, doi:10.1007/BF00208902.
Water-vapor transport from low to high latitudes in a given ocean and from one ocean to another must be compensated by a net flow of salt through the sea. A comparison is presented which shows that water-vapor fluxes derived from meteorological information, from an atmospheric general circulation model and from a radiocarbon-calibrated ocean box model are in first-order agreement.
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Broecker, W.S., Peng, T.-H., Jouzel, J., and Russell, G.: The magnitude of global fresh-water transports of importance to ocean circulation, Clim. Dynam., 4, 73-79, doi:10.1007/BF00208902, 1990.
Broecker, W.S., T.-H. Peng, J. Jouzel, and G. Russell (1990), The magnitude of global fresh-water transports of importance to ocean circulation, Clim. Dynam., 4, 73-79, doi:10.1007/BF00208902.
Broecker, W.S., T.-H. Peng, J. Jouzel, and G. Russell, 1990: The magnitude of global fresh-water transports of importance to ocean circulation. Clim. Dynam., 4, 73-79, doi:10.1007/BF00208902.
Broecker, W.S., Peng, T.-H., Jouzel, J., & Russell, G. 1990, Clim. Dynam., 4, 73, doi:10.1007/BF00208902.
Broecker WS, Peng T-H, Jouzel J, Russell G. The magnitude of global fresh-water transports of importance to ocean circulation, Clim Dynam 1990;4:73-79. doi:10.1007/BF00208902.
W.S. Broecker, T.-H. Peng, J. Jouzel, G. Russell, Clim. Dynam. 4, 73-79, doi:10.1007/BF00208902 (1990).
