Aura MLS

HOCl

Contact: Lucien Froidevaux

Although HOCl is not a major chlorine gas in terms of the atmospheric chlorine budget or ozone destruction, it does play some role in the chemical ozone destruction cycles and there are still significant uncertainties in its rate of formation (from ClO and HO2).

How it is part of MLS Science Objectives

Although HOCl is not a major chlorine gas in terms of the atmospheric chlorine budget or ozone destruction, it does play some role in the chemical ozone destruction cycles and there are still significant uncertainties in its rate of formation (from ClO and HO2). Obtaining global measurements of this product could help constrain some of these uncertainties.

How EOS MLS measures HOCl

The standard product for HOCl is taken from the 640 GHz retrievals. Simulations indicate that enhanced lower stratospheric values of 0.5 to 1 ppbv may be tracked at the 20% level, in single profiles. Real data systematics for HOCl, however, lead us to recommend a maximum pressure of 10 hPa.

HOCl is a noisy product and its typical stratospheric abundance is expected to be less than ~200 pptv, except under heterogeneously-enhanced conditions in the lower stratospheric winter polar vortex, where larger abundances of order 0.5 - 1 ppbv may occasionally be found.

We feel that zonal mean information (e.g., in 10°-wide bins) from one day's worth of MLS data is marginally useful, although monthly or bi-weekly averages will reduce the noise to more practical levels.

MLS values show a reasonable behavior in the upper stratosphere but have a tendency to be somewhat lower than other data (balloon data), and lower also (from a rough comparison) than the MIPAS published values (Von Clarmann et al., JGR, 2006) for Sep./Oct. 2002. More progress in the MLS retrievals for HOCl may come from (off-line) retrievals using averaged radiances or other methods in the future.

HOCl Information from the Spectroscopy Database

Quick Product Information for data version v5

  • Swath Name: HOCl
  • Status Flag: Only use profiles for which the Status field is an even number.
  • Useful Range: 10 - 2.2 hPa
  • DAAC Short Name: ML2HOCL
  • Precision: Only use values for which the estimated precision is a positive number.
  • Quality Threshold: >1.2
  • Convergence Threshold: <1.05

Download Aura MLS HOCl v5 data

Latest Publications (HOCl)

  1. Froidevaux, L., D. Kinnison, M. Santee, L. Millán, N. Livesey, W. Read, C. Bardeen, J. Orlando and R. Fuller
    Upper stratospheric ClO and HOCl trends (2005-2020): Aura Microwave Limb Sounder and model results
    Atmos. Chem. Phys. 10.5194/acp-22-4779-2022, 2022
  2. Hegglin, M., S. Tegtmeier, J. Anderson, A. Bourassa, S. Brohede, D. Degenstein, L. Froidevaux, B. Funke, J. Gille, Y. Kasai, E. Kyrölä, J. Lumpe, D. Murtagh, J. Neu, K. Pérot, E. Remsberg, A. Rozanov, M. Toohey, J. Urban, T. von Clarmann, K. Walker, H. Wang, C. Arosio, R. Damadeo, R. Fuller, G. Lingenfelser, C. McLinden, D. Pendlebury, C. Roth, N. Ryan, C. Sioris, L. Smith and K. Weigel
    Overview and update of the SPARC Data Initiative: comparison of stratospheric composition measurements from satellite limb sounders
    Earth System Science Data doi:10.5194/essd-13-1855-2021, 2021
  3. Häkkilä, T., P. Verronen, L. Millán, M. Szeląg, N. Kalakoski and A. Kero
    Odd hydrogen response thresholds for indication of solar proton and electron impact in the mesosphere and stratosphere
    Annales Geophysicae 10.5194/angeo-38-1299-2020, 2020
  4. Hegglin, M., S. Tegtmeier, J. Anderson, A. Bourassa, S. Brohede, D. Degenstein, L. Froidevaux, B. Funke, J. Gille, A. Jones, Y. Kasai, E. Kyrola, J. Lumpe, J. Neu, E. Remsberg, A. Rozanov, M. Toohey, J. Urban, T. von Clarmann, K.A. Walker and R. Wang
    The SPARC Data Initiative: Assessment of stratospheric trace gas and aerosol climatologies from satellite limb sounders
  5. Khosravi, M., P. Baron, J. Urban, L. Froidevaux, A.I. Jonsson, Y. Kasai, K. Kuribayashi, C. Mitsuda, D.P. Murtagh, H. Sagawa, M.L. Santee, T.O. Sato, M. Shiotani, M. Suzuki, T. von Clarmann, K.A. Walker and S. Wang
    Diurnal variation of stratospheric and lower mesospheric HOCl, ClO and HO2 at the equator: comparison of 1-D model calculations with measurements by satellite instruments
    Atmos. Chem. Phys. doi:10.5194/acp-13-7587-2013, 2013
  6. Damiani, A., B. Funke, D.R. Marsh, M. Lopez-Puertas, M.L. Santee, L. Froidevaux, S. Wang, C.H. Jackman, T. von Clarmann, A. Gardini, R.R. Cordero and M. Storini
    Impact of January 2005 solar proton events on chlorine species
    Atmos. Chem. Phys. doi:10.5194/acp-12-4159-2012, 2012
  7. Cofield, R.E. and P.C. Stek
    Design and field-of-view calibration of 114-660 GHz optics of the Earth Observing System Microwave Limb Sounder
    IEEE Trans. Geosci. Remote Sensing doi:10.1109/TGRS.2006.873234, 2006