A statistical method for testing a general circulation model with spectrally resolved satellite data

The motivation for this paper is to understand better the means available for testing climate models. Statistics of observed, outgoing, thermal spectra are compared with those predicted from a climate model, on the basis of data collected over a period of approximately 1 year. This is a powerful approach to testing a model with respect to processes internal to the atmosphere. These processes, which have characteristic timescales of less than a year, define the atmosphere's response to external forcing. Second-moment statistics are particularly important for testing model variability, which is key to predicting the results of forcing the atmosphere, for example, by ocean surface temperature changes, increase of greenhouse gases, etc. Comparisons are presented between statistical data from the infrared interferometer spectrometer (IRIS), an orbiting fourier transform spectrometer, and spectra calculated using the medium-resolution spectral code, MODTRAN, applied to the temperature and humidity profiles from a well-known climate model. Ten months of IRIS data are available, and we have compared means, standard deviations, skew, and kurtosis of its spectrally resolved brightness temperature in three tropical regions for individual months and for a range of timescales. Also presented are comparisons of covariances using Empirical Orthogonal Functions (EOFs) calculated in frequency space. All data that are presented are based on radiance differences from two like spectra, which eliminates many of the errors generated by the use of MODTRAN and most of the errors due to calibration uncertainties in IRIS. Important differences (i.e., residuals) between the IRIS and the GCM statistics are found in comparisons, demonstrating that the spectral data can provide a severe test of many aspects of the variability of a general circulation model. We discuss some of the residuals and how they may be used to improve model performance in the context of an adjoint formalism. In the long run the only way to have confidence in the performance of a model is to subject it to as many discriminating comparisons with data as are practicable, and we present a good candidate.

[1]  F. X. Kneizys,et al.  Users Guide to LOWTRAN 7 , 1988 .

[2]  Shepard A. Clough,et al.  Application of infrared interferometer spectrometer clear sky spectral radiance to investigations of climate variability , 1996 .

[3]  M. Iacono,et al.  Line‐by‐line calculation of atmospheric fluxes and cooling rates: 2. Application to carbon dioxide, ozone, methane, nitrous oxide and the halocarbons , 1995 .

[4]  W. Gates AMIP: The Atmospheric Model Intercomparison Project. , 1992 .

[5]  T. Barnett,et al.  Comparison of cloud fields from atmospheric general circulation model, in situ and satellite measurements , 1995 .

[6]  M. Chou Coolness in the tropical Pacific during an El Nino episode , 1994 .

[7]  Richard W. Reynolds,et al.  A Real-Time Global Sea Surface Temperature Analysis , 1988 .

[8]  Wedad A. Abdou,et al.  Detection of climate forcing using emission spectra , 1995 .

[9]  M. Webb,et al.  The spectral signature of global warming , 1997 .

[10]  kwang-yul kim,et al.  Detection of Forced Climate Signals. Part 1: Filter Theory , 1995 .

[11]  K. Hasselmann Optimal Fingerprints for the Detection of Time-dependent Climate Change , 1993 .

[12]  Makiko Sato,et al.  Potential climate impact of Mount Pinatubo eruption , 1992 .

[13]  R. Lindzen Can increasing carbon dioxide cause climate change? , 1997, Proceedings of the National Academy of Sciences of the United States of America.

[14]  Michael E. Schlesinger,et al.  Detecting changes in global climate induced by greenhouse gases , 1987 .

[15]  N Oreskes,et al.  Verification, Validation, and Confirmation of Numerical Models in the Earth Sciences , 1994, Science.

[16]  Vincent V. Salomonson,et al.  The Nimbus 4 infrared spectroscopy experiment: 1. Calibrated thermal emission spectra , 1972 .

[17]  Ilya Polyak Observed versus Simulated Second-Moment Climate Statistics in GCM Verification , 1996 .

[18]  Dan G. Cacuci,et al.  Physical Interpretation of the Adjoint Functions for Sensitivity Analysis of Atmospheric Models , 1983 .

[19]  T. Barnett Detection of changes in the global troposphere temperature field induced by greenhouse gases , 1986 .