DIAL and GNSS observations of the diurnal water‐vapour cycle above Iqaluit, Nunavut

• Published in: Quarterly Journal of the Royal Meteorological Society
• Main Authors: Hicks–Jalali, Shannon, Mariani, Zen, Crawford, Robert W.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2021
• Subjects: Arctic; Nunavut; Iqaluit
• Online Access: http://dx.doi.org/10.1002/qj.4175; https://onlinelibrary.wiley.com/doi/pdf/10.1002/qj.4175; https://onlinelibrary.wiley.com/doi/full-xml/10.1002/qj.4175; https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.4175

Abstract Atmospheric water vapour is the dominant gas in the greenhouse effect and its diurnal cycle is an essential component of the hydrological cycle. High‐quality water‐vapour measurements are critical observations for numerical weather prediction (NWP) models, which encounter difficulties in the Arctic due to its unique weather. Accurate measurements of the diurnal water‐vapour cycle can improve precipitation rate and type predictions. In this study, we use a preproduction Vaisala broad‐band differential absorption lidar (DIAL), installed in Iqaluit, Nunavut (63.75°N, 68.55°W), to calculate seasonal height‐resolved diurnal water‐vapour cycles from 100–1,500 m altitude. We also calculate the surface water‐vapour mixing ratio and integrated water‐vapour (IWV) diurnal cycles using co‐located surface station and global navigation satellite system (GNSS) measurements. We find that the first 250 m of the DIAL water‐vapour mixing ratio height‐resolved diurnal cycle agrees within 0.02 gkg with the surface‐station amplitudes, and within 0–2 hr in phase. DIAL diurnal‐cycle values are close to 1 at the surface, and between 0.25 and 0.95 depending on the altitude and season. The phases of the diurnal cycle shift and the amplitudes increase with altitude. In the summer, all instruments observe a strong 24‐hr cycle. The amplitude of the 24‐hr component decreases with the solar cycle, such that the 12‐hr component begins to influence the total cycle significantly by the winter. The IWV has a large 12‐hr component throughout the year, which could be due to the superposition of two diurnal components at different altitudes or increasing contributions at altitudes higher than those measured by the DIAL. We have shown that using DIAL measurements to observe height‐resolved diurnal cycles provides a deeper understanding of the diurnal cycle than that achieved from GNSS and surface measurements alone.