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Volume 9, issue 9
Atmos. Meas. Tech., 9, 4447-4457, 2016
https://doi.org/10.5194/amt-9-4447-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Water vapour in the upper troposphere and middle atmosphere:...

Atmos. Meas. Tech., 9, 4447-4457, 2016
https://doi.org/10.5194/amt-9-4447-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 08 Sep 2016

Research article | 08 Sep 2016

Recent divergences in stratospheric water vapor measurements by frost point hygrometers and the Aura Microwave Limb Sounder

Dale F. Hurst1,2, William G. Read3, Holger Vömel4, Henry B. Selkirk5,6, Karen H. Rosenlof7, Sean M. Davis1,7, Emrys G. Hall1,2, Allen F. Jordan1,2, and Samuel J. Oltmans1,2 Dale F. Hurst et al.
  • 1Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado, USA
  • 2Global Monitoring Division, NOAA Earth System Research Laboratory, Boulder, Colorado, USA
  • 3Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA
  • 4Earth Observing Laboratory, National Center for Atmospheric Research, Boulder, Colorado, USA
  • 5Laboratory for Atmospheric Chemistry and Dynamics, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
  • 6Goddard Earth Science Technology and Research, Universities Space Research Association, Columbia, Maryland, USA
  • 7Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, Colorado, USA

Abstract. Balloon-borne frost point hygrometers (FPs) and the Aura Microwave Limb Sounder (MLS) provide high-quality vertical profile measurements of water vapor in the upper troposphere and lower stratosphere (UTLS). A previous comparison of stratospheric water vapor measurements by FPs and MLS over three sites – Boulder, Colorado (40.0°N); Hilo, Hawaii (19.7°N); and Lauder, New Zealand (45.0°S) – from August 2004 through December 2012 not only demonstrated agreement better than 1% between 68 and 26hPa but also exposed statistically significant biases of 2 to 10% at 83 and 100hPa (Hurst et al., 2014). A simple linear regression analysis of the FP–MLS differences revealed no significant long-term drifts between the two instruments. Here we extend the drift comparison to mid-2015 and add two FP sites – Lindenberg, Germany (52.2°N), and San José, Costa Rica (10.0°N) – that employ FPs of different manufacture and calibration for their water vapor soundings. The extended comparison period reveals that stratospheric FP and MLS measurements over four of the five sites have diverged at rates of 0.03 to 0.07ppmvyear−1 (0.6 to 1.5%year−1) from  ∼ 2010 to mid-2015. These rates are similar in magnitude to the 30-year (1980–2010) average growth rate of stratospheric water vapor ( ∼ 1%year−1) measured by FPs over Boulder (Hurst et al., 2011). By mid-2015, the FP–MLS differences at some sites were large enough to exceed the combined accuracy estimates of the FP and MLS measurements.

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This study compares stratospheric water vapor measurements by the Aura Microwave Limb Sounder (MLS) and balloon-borne frost point hygrometers (FPs) at five sites that launch two different types of FPs. The results demonstrate that FP and MLS measurements have been diverging at statistically significant rates of 0.6 to 1.5 % per year since approximately 2010. Similarities in the divergences at different sites suggest a positive drift in MLS retrievals since approximately 2010.
This study compares stratospheric water vapor measurements by the Aura Microwave Limb Sounder...
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