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. , Jr., 1987 : Digital Spectral Analysis with Applications . Prentice Hall, 492 pp. Masson, V. , and Coauthors , 2008 : The Canopy and Aerosol Particles Interactions in Toulouse Urban Layer (CAPITOUL) Experiment . Meteor. Atmos. Phys. , 102 , 135 – 157 . Meijninger, W. M. L. , Beyrich F. , Lüdi A. , Kohsiek W. , and Bruin H. A. R. D. , 2005 : Scintillometer-based turbulent fluxes of sensible and latent heat over a heterogeneous land surface—A contribution to LITFASS-2003 . Bound
. , Jr., 1987 : Digital Spectral Analysis with Applications . Prentice Hall, 492 pp. Masson, V. , and Coauthors , 2008 : The Canopy and Aerosol Particles Interactions in Toulouse Urban Layer (CAPITOUL) Experiment . Meteor. Atmos. Phys. , 102 , 135 – 157 . Meijninger, W. M. L. , Beyrich F. , Lüdi A. , Kohsiek W. , and Bruin H. A. R. D. , 2005 : Scintillometer-based turbulent fluxes of sensible and latent heat over a heterogeneous land surface—A contribution to LITFASS-2003 . Bound
resolution under all weather conditions ( Gutman et al. 2004 ). Also, unlike microwave satellite retrievals, GPS can provide accurate water vapor estimates over land. Peixoto and Oort (1992) showed that approximately 80% of the water vapor in the Northern Hemisphere atmosphere at midlatitudes exists in the lowest 700 mb, so IWV serves as a good proxy for the low-level moisture that fuels precipitation. For example, using four winters of IWV measurements collected on the northern coast of California
resolution under all weather conditions ( Gutman et al. 2004 ). Also, unlike microwave satellite retrievals, GPS can provide accurate water vapor estimates over land. Peixoto and Oort (1992) showed that approximately 80% of the water vapor in the Northern Hemisphere atmosphere at midlatitudes exists in the lowest 700 mb, so IWV serves as a good proxy for the low-level moisture that fuels precipitation. For example, using four winters of IWV measurements collected on the northern coast of California
