AMT paper Weaver et al. 2018 in review
Comparison of ground-based and satellite measurements of water vapour vertical profiles over Ellesmere Island, Nunavut
Weaver, D., Strong, K., Walker, K. A., Sioris, C., Schneider, M., McElroy, C. T., Vömel, H., Sommer, M., Weigel, K., Rozanov, A., Burrows, J. P., Read, W. G., Fishbein, E., and Stiller, G.
by Atmospheric Measurement Techniques (AMT) at 2018-10-08, in review
Improving measurements of water vapour in the lower stratosphere and upper troposphere (UTLS) is a priority for the atmospheric science community. In this work, UTLS water vapour profiles derived from Atmospheric Chemistry Experiment (ACE) satellite measurements are assessed with coincident ground-based measurements taken at a high Arctic observatory at Eureka, Nunavut, Canada. Additional comparisons to satellite measurements taken by AIRS, MIPAS, MLS, SCIAMACHY, and TES are included to put the ACE-FTS and ACE-MAESTRO results in context.
Measurements of water vapour profiles at Eureka are made using a Bruker 125HR solar absorption Fourier transform infrared spectrometer at the Polar Environment Atmospheric Research Laboratory (PEARL) and radiosondes launched from the Eureka Weather Station. Radiosonde measurements used in this study have been processed with software developed by the Global Climate Observing System (GCOS) Reference Upper Air Network (GRUAN) to account for known biases and calculate uncertainties in a well-documented and consistent manner.
ACE-FTS measurements were within 11ppmv (13%) of 125HR measurements between 6 and 14km. Between 8 and 14km ACE-FTS profiles showed a small wet bias of approximately 8% relative to the 125HR. ACE-FTS water vapour profiles had mean differences of 13ppmv (32%) or better when compared to coincident radiosonde profiles at altitudes between 6 and 14km; mean differences were within 6ppmv (12%) between 7 and 11km. ACE-MAESTRO profiles showed a small dry bias relative to the 125HR of approximately 7% between 6 and 9km and 10% between 10 and 14km. ACE-MAESTRO profiles agreed within 30ppmv (36%) of the radiosondes between 7 and 14km. ACE-FTS and ACE-MAESTRO comparison results show closer agreement with the radiosondes and PEARL 125HR overall than other satellite datasets – except AIRS. Close agreement was observed between AIRS and the 125HR and radiosonde measurements, with mean differences within 5% and correlation coefficients above 0.83 in the troposphere between 1 and 7km.
Comparisons to MLS at altitudes around 10km showed a dry bias, e.g., mean differences between MLS and radiosondes were −25.6%. SCIAMACHY comparisons were very limited due to minimal overlap between the vertical extent of the measurements. TES had no temporal overlap with the radiosonde dataset used in this study. Comparisons between TES and the 125HR showed a wet bias of approximately 25% in the UTLS and mean differences within 14% below 5km.
Weaver, D., Strong, K., Walker, K. A., Sioris, C., Schneider, M., McElroy, C. T., Vömel, H., Sommer, M., Weigel, K., Rozanov, A., Burrows, J. P., Read, W. G., Fishbein, E., and Stiller, G.: Comparison of ground-based and satellite measurements of water vapour vertical profiles over Ellesmere Island, Nunavut, Atmos. Meas. Tech. Discuss., https://doi.org/10.5194/amt-2018-267, in review, 2018.