Intercomparison of atmospheric water vapour measurements at a Canadian High Arctic site

  • Dan Weaver
  • , Kimberly Strong
  • , Matthias Schneider
  • , Penny M. Rowe
  • , Chris Sioris
  • , Kaley A. Walker
  • , Zen Mariani
  • , Taneil Uttal
  • , C. Thomas McElroy
  • , Holger Vömel
  • , Alessio Spassiani
  • , James R. Drummond

Research output: Contribution to journalArticlepeer-review

18 Scopus citations

Abstract

Water vapour is a critical component of the Earth system. Techniques to acquire and improve measurements of atmospheric water vapour and its isotopes are under active development. This work presents a detailed intercomparison of water vapour total column measurements taken between 2006 and 2014 at a Canadian High Arctic research site (Eureka, Nunavut). Instruments include radiosondes, sun photometers, a microwave radiometer, and emission and solar absorption Fourier transform infrared (FTIR) spectrometers. Close agreement is observed between all combination of datasets, with mean differences ≤1.0 kgm-2 and correlation coefficients ≥0.98. The one exception in the observed high correlation is the comparison between the microwave radiometer and a radiosonde product, which had a correlation coefficient of 0.92. A variety of biases affecting Eureka instruments are revealed and discussed. A subset of Eureka radiosonde measurements was processed by the Global Climate Observing System (GCOS) Reference Upper Air Network (GRUAN) for this study. Comparisons reveal a small dry bias in the standard radiosonde measurement water vapour total columns of approximately 4 %. A recently produced solar absorption FTIR spectrometer dataset resulting from the MUSICA (MUlti-platform remote Sensing of Isotopologues for investigating the Cycle of Atmospheric water) retrieval technique is shown to offer accurate measurements of water vapour total columns (e.g. average agreement within-5.2% of GRUAN and-6.5% of a co-located emission FTIR spectrometer). However, comparisons show a small wet bias of approximately 6% at the high-latitude Eureka site. In addition, a new dataset derived from Atmospheric Emitted Radiance Interferometer (AERI) measurements is shown to provide accurate water vapour measurements (e.g. average agreement was within 4% of GRUAN), which usefully enables measurements to be taken during day and night (especially valuable during polar night).

Original languageEnglish
Pages (from-to)2851-2880
Number of pages30
JournalAtmospheric Measurement Techniques
Volume10
Issue number8
DOIs
StatePublished - Aug 11 2017
Externally publishedYes

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