Search Results

You are looking at 1 - 2 of 2 items for :

  • Atmosphere-land interactions x
  • 16th International Symposium for the Advancement of Boundary-Layer Remote Sensing (ISARS 2012) x
  • All content x
Clear All
C. R. Wood, R. D. Kouznetsov, R. Gierens, A. Nordbo, L. Järvi, M. A. Kallistratova, and J. Kukkonen

. , 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

Full access
A. B. White, M. L. Anderson, M. D. Dettinger, F. M. Ralph, A. Hinojosa, D. R. Cayan, R. K. Hartman, D. W. Reynolds, L. E. Johnson, T. L. Schneider, R. Cifelli, Z. Toth, S. I. Gutman, C. W. King, F. Gehrke, P. E. Johnston, C. Walls, D. Mann, D. J. Gottas, and T. Coleman

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

Full access