The advective transport of atmospheric water vapor, its role in global
hydrology, and the water balance of continental regions are discussed
and explored. A data set consisting of 10 years of global wind and hu
midity observations that has been interpolated onto a regular grid is
used to estimate atmospheric water vapor fluxes across the boundaries
of selected continental regions. The flux of water vapor from the wate
rs surrounding the Americas is computed and graphically represented as
integrated normal flux across meridional and zonal segments. The tota
l flux is decomposed into transport by mean motion and transport by co
rrelated transient anomalies in the wind and humidity fields. Seasonal
maps of these observations for the Americas reveal the underlying mec
hanisms and illustrate the characterizing features of the hydrologic c
ycle and continental water balance for this large land mass.