| Literature DB >> 33619291 |
Edgardo Sepúlveda1, Raul R Cordero2, Alessandro Damiani3, Sarah Feron4,5, Jaime Pizarro1, Felix Zamorano6, Rigel Kivi7, Ricardo Sánchez8, Margarita Yela9, Julien Jumelet10, Alejandro Godoy8, Jorge Carrasco6, Juan S Crespo11, Gunther Seckmeyer12, Jose A Jorquera1, Juan M Carrera1, Braulio Valdevenito1, Sergio Cabrera13, Alberto Redondas14, Penny M Rowe1,15.
Abstract
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.Entities:
Year: 2021 PMID: 33619291 PMCID: PMC7900121 DOI: 10.1038/s41598-021-81954-6
Source DB: PubMed Journal: Sci Rep ISSN: 2045-2322 Impact factor: 4.379