Comparison of Electrochemical Concentration Cell Ozonesonde and Microwave Limb Sounder Satellite Remote Sensing Ozone Profiles for the Center of the South Asian High

To further verify the ozone profile reliability of satellite remote sensing for the ozone valley over the Tibetan Plateau in the core area of the South Asian high in summer, we validate the ozone products from the microwave limb sounder (MLS) onboard the Aura satellite over the Tibetan plateau using electrochemical concentration cell (ECC) ozonesonde data of 2016 for Ngari, Tibet. The MLS version four ozone profiles have lower standard deviation in the middle stratosphere (38–10 hPa), whereas the ozonesonde profiles have lower standard deviation in the upper troposphere and lower stratosphere region (200–83 hPa). There are statistically significant differences between these two datasets in most of the stratosphere (10–83 hPa). The mean value of MLS ozone is about 0.8–1.5 mPa greater than that of ECC ozone, which corresponds to a relative deviation of 59 ± 24% at 83 hPa, 24 ± 13% at 68 hPa, 20 ± 5% at 56 hPa, 14 ± 4% at 46 hPa and 38 hPa, and 9 ± 4% in the layers between 32 and 10 hPa. However, there is no statistically significant difference between the two datasets in the upper troposphere (100–200 hPa).

[1]  Xiuji Zhou,et al.  Dynamic effects of the South Asian high on the ozone valley over the Tibetan Plateau , 2012, Acta Meteorologica Sinica.

[2]  Gert König-Langlo,et al.  Validation of Aura Microwave Limb Sounder Ozone by ozonesonde and lidar measurements , 2007 .

[3]  Xiuji Zhou,et al.  Evaluation of the trend uncertainty in summer ozone valley over the Tibetan Plateau in three reanalysis datasets , 2017, Journal of Meteorological Research.

[4]  X. Liang,et al.  A Case Study of Mass Transport during the East-West Oscillation of the Asian Summer Monsoon Anticyclone , 2017 .

[5]  C. Rodgers Characterization and Error Analysis of Profiles Retrieved From Remote Sounding Measurements , 1990 .

[6]  A. Thompson,et al.  Assessment of the performance of ECC‐ozonesondes under quasi‐flight conditions in the environmental simulation chamber: Insights from the Juelich Ozone Sonde Intercomparison Experiment (JOSIE) , 2007 .

[7]  Jianjun Xu,et al.  Double core of ozone valley over the Tibetan Plateau and its possible mechanisms , 2015 .

[8]  H. Vömel,et al.  In situ water vapor and ozone measurements in Lhasa and Kunming during the Asian summer monsoon , 2012 .

[9]  James M. Russell,et al.  The Halogen Occultation Experiment , 1993 .

[10]  Wei Li,et al.  Validation of Aura Microwave Limb Sounder water vapor and ozone profiles over the Tibetan Plateau and its adjacent region during boreal summer , 2015, Science China Earth Sciences.

[11]  S. Massie,et al.  Formation of the summertime ozone valley over the Tibetan Plateau: The Asian summer monsoon and air column variations , 2011 .

[12]  A. Thompson,et al.  First reprocessing of Southern Hemisphere ADditional OZonesondes (SHADOZ) profile records (1998–2015): 1. Methodology and evaluation , 2017 .

[13]  J. Thepaut,et al.  The ERA‐Interim reanalysis: configuration and performance of the data assimilation system , 2011 .

[14]  L. E. Mauldin,et al.  Stratospheric Aerosol And Gas Experiment II Instrument: A Functional Description , 1985 .

[15]  Shunwu Zhou,et al.  Impact of Ozone Valley over the Tibetan Plateau on the South Asian High in CAM5 , 2017 .

[16]  T. Clarmann Validation of remotely sensed profiles of atmospheric state variables: strategies and terminology , 2006 .

[17]  Peter H. Siegel,et al.  The Earth observing system microwave limb sounder (EOS MLS) on the aura Satellite , 2006, IEEE Transactions on Geoscience and Remote Sensing.

[18]  Robert A. Barnes,et al.  Electrochemical concentration cell ozonesonde performance evaluation during STOIC 1989 , 1995 .

[19]  Stanley Bruckenstein,et al.  Electrochemical Kinetics: Theoretical and Experimental Aspects , 1967 .

[20]  Jonathon S. Wright,et al.  Validation of Aura MLS retrievals of temperature, water vapour and ozone in the upper troposphere and lower-middle stratosphere over the Tibetan Plateau during boreal summer , 2016 .