Atmospheric Measurement Techniques (Jun 2014)

Evaluation of the airborne quantum cascade laser spectrometer (QCLS) measurements of the carbon and greenhouse gas suite &ndash; CO<sub>2</sub>, CH<sub>4</sub>, N<sub>2</sub>O, and CO &ndash; during the CalNex and HIPPO campaigns

  • G. W. Santoni,
  • B. C. Daube,
  • E. A. Kort,
  • R. Jiménez,
  • S. Park,
  • J. V. Pittman,
  • E. Gottlieb,
  • B. Xiang,
  • M. S. Zahniser,
  • D. D. Nelson,
  • J. B. McManus,
  • J. Peischl,
  • T. B. Ryerson,
  • J. S. Holloway,
  • A. E. Andrews,
  • C. Sweeney,
  • B. Hall,
  • E. J. Hintsa,
  • F. L. Moore,
  • J. W. Elkins,
  • D. F. Hurst,
  • B. B. Stephens,
  • J. Bent,
  • S. C. Wofsy

DOI
https://doi.org/10.5194/amt-7-1509-2014
Journal volume & issue
Vol. 7, no. 6
pp. 1509 – 1526

Abstract

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We present an evaluation of aircraft observations of the carbon and greenhouse gases CO2, CH4, N2O, and CO using a direct-absorption pulsed quantum cascade laser spectrometer (QCLS) operated during the HIPPO and CalNex airborne experiments. The QCLS made continuous 1 Hz measurements with 1σ Allan precisions of 20, 0.5, 0.09, and 0.15 ppb for CO2, CH4, N2O, and CO, respectively, over > 500 flight hours on 79 research flights. The QCLS measurements are compared to two vacuum ultraviolet (VUV) CO instruments (CalNex and HIPPO), a cavity ring-down spectrometer (CRDS) measuring CO2 and CH4 (CalNex), two broadband non-dispersive infrared (NDIR) spectrometers measuring CO2 (HIPPO), two onboard gas chromatographs measuring a variety of chemical species including CH4, N2O, and CO (HIPPO), and various flask-based measurements of all four species. QCLS measurements are tied to NOAA and WMO standards using an in-flight calibration system, and mean differences when compared to NOAA CCG flask data over the 59 HIPPO research flights were 100, 1, 1, and 2 ppb for CO2, CH4, N2O, and CO, respectively. The details of the end-to-end calibration procedures and the data quality assurance and quality control (QA/QC) are presented. Specifically, we discuss our practices for the traceability of standards given uncertainties in calibration cylinders, isotopic and surface effects for the long-lived greenhouse gas tracers, interpolation techniques for in-flight calibrations, and the effects of instrument linearity on retrieved mole fractions.