Evaluation of Antarctic Ozone Profiles derived from OMPS-LP by using Balloon-borne Ozonesondes
Sepulveda, Edgardo
Universidad de Santiago de Chile
Cordero, Raul R.
Universidad de Santiago de Chile
Damiani, Alessandro
Chiba University
Feron, Sarah
Universidad de Santiago de Chile
Pizarro, Jaime
Universidad de Santiago de Chile
Kivi, Rigel
Finnish Meteorological Institute
Sanchez, Ricardo
Serv Meteorol Nacl
Yela, Margarita
Inst Nacl Tecn Aeroesp INTA
Jumelet, Julien
Universite Paris Saclay
Godoy, Alejandro
Serv Meteorol Nacl
Crespo, Juan S.
Direcc Meteorol Chile
Seckmeyer, Gunther
Leibniz University Hannover
Jorquera, Jose A.
Universidad de Santiago de Chile
Carrera, Juan M.
Universidad de Santiago de Chile
Valdevenito, Braulio
Universidad de Santiago de Chile
Cabrera, Sergio
Universidad de Chile
Redondas, Alberto
Agencia Estatal de Meteorologia (AEMET)
Rowe, Penny M.
Universidad de Santiago de Chile
Journal
Scientific Reports
ISSN
2045-2322
Open Access
gold
Volume
11
Predicting radiative forcing due to Antarctic stratospheric ozone recovery requires detecting changes in the ozone vertical distribution. In this endeavor, the Limb Profiler of the Ozone Mapping and Profiler Suite (OMPS-LP), aboard the Suomi NPP satellite, has played a key role providing ozone profiles over Antarctica since 2011. Here, we compare ozone profiles derived from OMPS-LP data (version 2.5 algorithm) with balloon-borne ozonesondes launched from 8 Antarctic stations over the period 2012-2020. Comparisons focus on the layer from 12.5 to 27.5 km and include ozone profiles retrieved during the Sudden Stratospheric Warming (SSW) event registered in Spring 2019. We found that, over the period December-January-February-March, the root mean square error (RMSE) tends to be larger (about 20%) in the lower stratosphere (12.5-17.5 km) and smaller (about 10%) within higher layers (17.5-27.5 km). During the ozone hole season (September-October-November), RMSE values rise up to 40% within the layer from 12.5 to 22 km. Nevertheless, relative to balloon-borne measurements, the mean bias error of OMPS-derived Antarctic ozone profiles is generally lower than 0.3 ppmv, regardless of the season.
Name
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Type
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Format
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