The Full-spectrum Correlated K Method for Longwave Atmosphic Radiative Transfer: Treatment of Gaseous Overlap

Robin Hogan University of Reading

Category: Radiation

Working Group: Cloud Life Cycle

Image Thumbnail
Evaluation of the 23- and 32-point FSCK models on four different McClatchey et al. (1972) standard atmospheres (indicated by the legend in panel d, where MLS is the mid-latitude summer atmosphere and SAW is the sub-arctic winter atmosphere) containing only H2O, CO2, and O3. (a) Longwave heating rate calculated at full spectral resolution, (b) the error in heating rate of the 23-point FSCK model, (c) the error in heating rate of the 32-point FSCK model, and (d)–(f) the same but for net longwave flux (upwelling minus downwelling).

The correlated k-distribution (CKD) method is widely used in the radiative transfer schemes of atmospheric models and involves dividing the spectrum into a number of bands and then reordering the gaseous absorption coefficients within each one. The fluxes and heating rates for each band may then be computed by discretizing the reordered spectrum into of order 10 quadrature points per major gas and performing a monochromatic radiation calculation for each point. In this poster it is shown that for clear-sky longwave calculations, sufficient accuracy for most applications can be achieved without the need for bands: reordering may be performed on the entire longwave spectrum. The resulting full-spectrum correlated k (FSCK) method requires significantly fewer monochromatic calculations than standard CKD to achieve a given accuracy. The concept is first demonstrated by comparing with line-by-line calculations for an atmosphere containing only water vapor, in which it is shown that the accuracy of heating-rate calculations improves approximately in proportion to the square of the number of quadrature points. For more than around 20 points, the root-mean-squared error flattens out at around 0.015 K/day due to the imperfect rank correlation of absorption spectra at different pressures in the profile. The spectral overlap of m different gases is treated by considering an m-dimensional hypercube where each axis corresponds to the reordered spectrum of one of the gases. This hypercube is then divided up into a number of volumes, each approximated by a single quadrature point, such that the total number of quadrature points is slightly fewer than the sum of the number that would be required to treat each of the gases separately. The gaseous absorptions for each quadrature point are optimized such that they minimize a cost function expressing the deviation of the heating rates and fluxes calculated by the FSCK method from line-by-line calculations for a number of training profiles. This approach is validated for atmospheres containing water vapor, carbon dioxide, and ozone, in which it is found that in the troposphere and most of the stratosphere, heating-rate errors of less than 0.2 K/day can be achieved using a total of 23 quadrature points, decreasing to less than 0.1 K/day for 32 quadrature points. It would be relatively straightforward to extend the method to include other gases.

http://www.met.reading.ac.uk/clouds/publications/fsck.pdf

This poster will be displayed at ASR Science Team Meeting.