Downward longwave radiation estimates for clear-sky conditions over northeast Brazil

The main objective of this paper is to assess the performance of nine downward longwave radiation equations for clear-sky condition and develop a locally adjusted equation using the observed vapor pressure and air temperature data. The radiation and atmospheric parameters were measured during the months of October 2005 to June 2006 at a micrometeorological tower installed at the experimental site in a banana orchard in the semiarid region of Northeast Brazil. The comparative statistics for the performance of the downward longwave radiation calculation models during daytime and nighttime compared to measured data have shown that the parameterizations with more physical foundations have the best results. The locally adjusted equation and Sugita and Brutsaert model developed in 1993 showed errors less than 1.0% in comparison with measured values. Downward longwave radiation is one of the most expensive and difficult component of the radiation budget to be monitored in micrometeorological studies. Hence, the locally adjusted equation can be used to estimate downward longwave energy, needed as input to some agricultural and hydrological models, in semi-arid regions of the Northeast Brazil, where this component is not monitored.

[1]  John H. C. Gash,et al.  Longwave Radiation from Clear Skies in Niger: A Comparison of Observations with Simple Formulas , 1993 .

[2]  William P. Kustas,et al.  Assessment of clear and cloudy sky parameterizations for daily downwelling longwave radiation over different land surfaces in Florida, USA , 2008 .

[3]  D. Brunt Notes on radiation in the atmosphere. I , 2007 .

[4]  S. Idso A set of equations for full spectrum and 8- to 14-μm and 10.5- to 12.5-μm thermal radiation from cloudless skies , 1981 .

[5]  K. I. Kondratʹev Radiation in the atmosphere , 1969 .

[6]  Ronald L. Elliott,et al.  On the development of a simple downwelling longwave radiation scheme , 2002 .

[7]  Finn Plauborg,et al.  Comparison of models for calculating daytime long-wave irradiance using long term data set , 2007 .

[8]  Sin Chan Chou,et al.  Downward longwave radiation estimates for clear and all-sky conditions in the Sertãozinho region of São Paulo, Brazil , 2010 .

[9]  W. Brutsaert,et al.  Cloud effect in the estimation of instantaneous downward longwave radiation , 1993 .

[10]  A. Prata A new long‐wave formula for estimating downward clear‐sky radiation at the surface , 1996 .

[11]  J. H. Shaw,et al.  Thermal Radiation from the Atmosphere , 1956 .

[12]  W. Swinbank Long‐wave radiation from clear skies , 1963 .

[13]  T. M. Crawford,et al.  An Improved Parameterization for Estimating Effective Atmospheric Emissivity for Use in Calculating Daytime Downwelling Longwave Radiation , 1999 .

[14]  C. Bohren,et al.  An introduction to atmospheric radiation , 1981 .

[15]  J. Monteith,et al.  Boundary Layer Climates. , 1979 .

[16]  N. L. Dias,et al.  Assessing daytime downward longwave radiation estimates for clear and cloudy skies in Southern Brazil , 2006 .

[17]  R. Stull An Introduction to Boundary Layer Meteorology , 1988 .

[18]  Gerald N. Flerchinger,et al.  Comparison of algorithms for incoming atmospheric long‐wave radiation , 2009 .