Research data supporting 'The double peak in upwelling and heating in the tropical lower stratosphere'.

The data is the ozone climatology from Fortuin and Langematz (1994) as it is used in the radiation code of the ECMWF IFS to generate the ERA-Interim reanalysis dataset (Dee et al. 2011). The data is in ppmv on 36 vertical levels and 19 latitudinal bands.This is then internally interpolated on the grid used by the model before entering radiation. References: Fortuin, J. P., and U. Langematz, 1994: Update on the global ozone climatology and on concurrent ozone and temperature trends. Proc. SPIE, Atmospheric Sensing and Modelling, R. P. Santer, Ed., Vol. 2311, 207–216, doi:10.1117/12.198578. Dee, D. P., and Coauthors, 2011: The ERA-Interim reanalysis: configuration and performance of the data assimilation system. Quarterly Journal of the Royal Meteorological Society, 137, 553–597, doi:10.1002/qj.828.

本数据集采用Fortuin与Langematz（1994）提出的臭氧气候学数据，该数据被用于欧洲中期天气预报中心（European Centre for Medium-Range Weather Forecasts, ECMWF）集成预报系统（Integrated Forecasting System, IFS）的辐射代码中，用于生成ERA-Interim再分析数据集（Dee等，2011）。该数据集以体积混合比（parts per million by volume, ppmv）为单位，包含36个垂直层与19个纬度带。随后该数据集会在进入辐射模块前，在数值模式所用的网格上完成内部插值。

参考文献：
1. Fortuin, J. P. 及 U. Langematz, 1994：全球臭氧气候学及同期臭氧与温度趋势的更新。见：《大气遥感与建模》，R. P. Santer 编辑，国际光学工程学会（SPIE）会议论文集，第2311卷，207–216页，DOI: 10.1117/12.198578。
2. Dee, D. P. 及合著者, 2011：ERA-Interim再分析数据集：数据同化系统的配置与性能。《皇家气象学会季刊》，第137卷，553–597页，DOI: 10.1002/qj.828。