Trend differences in lower stratospheric water vapour between Boulder and the zonal mean and their role in understanding fundamental observational discrepancies

• Published in: Atmospheric chemistry and physics 2018-06, Vol.18 (11), p.8331-8351
• Main Authors: Lossow, Stefan, Hurst, Dale F, Rosenlof, Karen H, Stiller, Gabriele P, von Clarmann, Thomas, Brinkop, Sabine, Dameris, Martin, Jöckel, Patrick, Kinnison, Doug E, Plieninger, Johannes, Plummer, David A, Ploeger, Felix, Read, William G, Remsberg, Ellis E, Russell, James M, Tao, Mengchu
• Format: Article
• Language: English
• Subjects: Altitude; Atmosphere; Atmospheric chemistry; Atmospheric models; Atmospheric research; Atmospheric sounding; Atmospheric water; Bias; Clams; Climate models; Cold; Computer simulation; Data; Datasets; Earth; Estimates; Halogen Occultation Experiment; Halogens; Hygrometers; Interferometers; Latitude; Measurement techniques; Michelson interferometers; Middle atmosphere; Modular systems; Observations; Organic chemistry; Properties; Satellite data; Satellite observation; Satellites; Simulation; Stratosphere; Stratospheric circulation; Temperature; Trends; Upper atmosphere; Water vapor; Water vapour; Weather forecasting
• ISSN: 1680-7324; 1680-7316; 1680-7324
• DOI: 10.5194/acp-18-8331-2018

Trend estimates with different signs are reported in the literature for lower stratospheric water vapour considering the time period between the late 1980s and 2010. The NOAA (National Oceanic and Atmospheric Administration) frost point hygrometer (FPH) observations at Boulder (Colorado, 40.0° N, 105.2° W) indicate positive trends (about 0.1 to 0.45 ppmv decade−1). On the contrary, negative trends (approximately −0.2 to −0.1 ppmv decade−1) are derived from a merged zonal mean satellite data set for a latitude band around the Boulder latitude. Overall, the trend differences between the two data sets range from about 0.3 to 0.5 ppmv decade−1, depending on altitude. It has been proposed that a possible explanation for these discrepancies is a different temporal behaviour at Boulder and the zonal mean. In this work we investigate trend differences between Boulder and the zonal mean using primarily simulations from ECHAM/MESSy (European Centre for Medium-Range Weather Forecasts Hamburg/Modular Earth Submodel System) Atmospheric Chemistry (EMAC), WACCM (Whole Atmosphere Community Climate Model), CMAM (Canadian Middle Atmosphere Model) and CLaMS (Chemical Lagrangian Model of the Stratosphere). On shorter timescales we address this aspect also based on satellite observations from UARS/HALOE (Upper Atmosphere Research Satellite/Halogen Occultation Experiment), Envisat/MIPAS (Environmental Satellite/Michelson Interferometer for Passive Atmospheric Sounding) and Aura/MLS (Microwave Limb Sounder). Overall, both the simulations and observations exhibit trend differences between Boulder and the zonal mean. The differences are dependent on altitude and the time period considered. The model simulations indicate only small trend differences between Boulder and the zonal mean for the time period between the late 1980s and 2010. These are clearly not sufficient to explain the discrepancies between the trend estimates derived from the FPH observations and the merged zonal mean satellite data set. Unless the simulations underrepresent variability or the trend differences originate from smaller spatial and temporal scales than resolved by the model simulations, trends at Boulder for this time period should also be quite representative for the zonal mean and even other latitude bands. Trend differences for a decade of data are larger and need to be kept in mind when comparing results for Boulder and the zonal mean on this timescale. Beyond that, we find that the trend estimates