A Comparison of Rainfall, Outgoing Longwave Radiation, and Divergence over the Amazon Basin

Brant Liebmann
Climate Diagnostics Center, University of Colorado, Boulder, Colorado

JosÚ A. Marengo, John D. Glick, Vernon E. Kousky, Ilana C. Wainer, and Oswaldo Massambani

(Manuscript received 26 June 1997, in final form 5 November 1997)


Observed rainfall, outgoing longwave radiation (OLR), and divergence and precipitation from the Reanalysis project of the National Centers for Environmental Prediction and Atmospheric Research are compared over the Amazon basin. The spatial pattern of the mean and the phase of the annual cycle generally compare well, except that the amplitude of the annual cycle of model precipitation is much smaller than observed. On 10 - 30 day time scales, it is shown that averaging stations with a 5░ radius is approximately equivalent to total wave number 20 (T20) spatial scale, although it is more important to have a high density of stations then an exact match of spatial scales. Ideally, there should be 1 station per 20,000 square kilometers. On 10 - 30 day scales, observed rainfall is best correlated with OLR. Correlations between OLR and 150 mb divergence are larger than between observed rainfall and divergence or between rainfall and model precipitation. For example, if 10-30 day filtered OLR and divergence are truncated at T20, and rainfall is averaged to include stations within a 5░ radius, OLR is correlated with rainfall at about -0.6, OLR is correlated with divergence at about -0.35, and rainfall is correlated with divergence at about 0.2. At least part of the lack of correlation is due to inadequate spatial sampling of rainfall. Correlations improve with larger spatial scale. The major seasonal transitions from dry to rainy regimes are captured well by OLR, but not by the model quantities. The mean diurnal cycle is represented reasonably by 150 mb divergence.