A 16-year global climate data record of total column water vapour generated from OMI observations in the visible blue spectral range

• Published in: Earth System Science Data
• Main Authors: Borger, Christian, Beirle, Steffen, Wagner, Thomas
• Format: Text
• Language: English
• Published: 2023
• Subjects: Antarc*; Antarctica
• Online Access: https://doi.org/10.5194/essd-15-3023-2023; https://essd.copernicus.org/articles/15/3023/2023/

We present a long-term data set of 1 ∘ × 1 ∘ <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="34pt" height="11pt" class="svg-formula" dspmath="mathimg" md5hash="18e249d247dd6d35235fb683ecd82671"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="essd-15-3023-2023-ie00001.svg" width="34pt" height="11pt" src="essd-15-3023-2023-ie00001.png"/></svg:svg> monthly mean total column water vapour (TCWV) based on global measurements of the Ozone Monitoring Instrument (OMI) covering the time range from January 2005 to December 2020. In comparison to the retrieval algorithm of Borger et al. ( 2020 ) , several modifications and filters have been applied accounting for instrumental issues (such as OMI's “row anomaly”) or the inferior quality of solar reference spectra. For instance, to overcome issues related to low-quality reference spectra, the daily solar irradiance spectrum is replaced by an annually varying mean earthshine radiance obtained in December over Antarctica. For the TCWV data set, we only consider measurements with an effective cloud fraction less than 20 %, an air mass factor (AMF) greater than 0.1, a snow- and ice-free ground pixel, and an OMI row that is not affected by the row anomaly over the complete time range of the data set. The individual TCWV measurements are then gridded to a regular 1 ∘ × 1 ∘ <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="34pt" height="11pt" class="svg-formula" dspmath="mathimg" md5hash="21fbad4d1955efadb851b48211f1f95d"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="essd-15-3023-2023-ie00002.svg" width="34pt" height="11pt" src="essd-15-3023-2023-ie00002.png"/></svg:svg> lattice, from which the monthly means are calculated. The investigation of sampling errors in the OMI TCWV data set shows that these are dominated by the clear-sky bias and cause on average deviations of around − 10 %, which is consistent with the findings of previous studies. However, the spatiotemporal sampling errors and those ...