NO2 VCD Stratospheric trends Hemispheric and latitudinal dependence

Presentación realizada para el 7th International DOAS Workshop celebrado en Bruselas los días 6-8 de julio de 2015 Twenty years of stratospheric NO2 VCD data from ground-based zenith DOAS instruments have been used for trend analysis. Spectrometers either NDACC qualified or under evaluation cover Su...

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Main Authors: Gil-Ojeda, Manuel, Yela González, Margarita, Navarro Comas, Mónica, Robles González, Cristina, Hase, F., Funke, Bernd, Puentedura, Olga, Iglesias, Javier, Cuevas Agulló, Emilio
Format: Conference Object
Language:English
Published: 2015
Subjects:
Online Access:https://hdl.handle.net/20.500.11765/1137
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author Gil-Ojeda, Manuel
Yela González, Margarita
Navarro Comas, Mónica
Robles González, Cristina
Hase, F.
Funke, Bernd
Puentedura, Olga
Iglesias, Javier
Cuevas Agulló, Emilio
author_facet Gil-Ojeda, Manuel
Yela González, Margarita
Navarro Comas, Mónica
Robles González, Cristina
Hase, F.
Funke, Bernd
Puentedura, Olga
Iglesias, Javier
Cuevas Agulló, Emilio
author_sort Gil-Ojeda, Manuel
collection ARCIMÍS (Archivo Climatológico y Meteorológico Institucional - AEMET, Agencia Estatal de Meteorología)
description Presentación realizada para el 7th International DOAS Workshop celebrado en Bruselas los días 6-8 de julio de 2015 Twenty years of stratospheric NO2 VCD data from ground-based zenith DOAS instruments have been used for trend analysis. Spectrometers either NDACC qualified or under evaluation cover Subtropical latitudes in Northern Hemisphere (Izaña, 28ºN), and Southern Antarctic (Marambio, 64ºS) and SubAntarctic (Ushuaia, 55ºS) regions. The multiple linear regression method includes annual, semiannual, quarterly, solar activity cycle, stratospheric aerosols, QBO and NAO proxies. The instruments settings follow the NDACC recommendations for NO2 measurements and the same AMF code. Results show a mean am/pm positive trend of + 7.9% at the 99% confidence level in the Northern Hemisphere station whereas the trends are negative in the Southern Hemisphere ones (-9.8% Ushuaia, -14.9% Marambio). From comparison with FTIR data, it is estimated that the changes are restricted to the lower stratosphere (15-30km) suggesting a dynamic origin of the trend. MIPAS NOy on a global scale shows a similar feature with a redistribution of the nitrogen family within the lower stratosphere.
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genre_facet Antarc*
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spelling ftaemet:oai:repositorio.aemet.es:20.500.11765/1137 2025-04-20T14:23:16+00:00 NO2 VCD Stratospheric trends Hemispheric and latitudinal dependence Gil-Ojeda, Manuel Yela González, Margarita Navarro Comas, Mónica Robles González, Cristina Hase, F. Funke, Bernd Puentedura, Olga Iglesias, Javier Cuevas Agulló, Emilio 2015 application/pdf https://hdl.handle.net/20.500.11765/1137 eng eng http://hdl.handle.net/20.500.11765/1137 Licencia CC: Reconocimiento–NoComercial–SinObraDerivada CC BY-NC-ND info:eu-repo/semantics/openAccess Espectrómetros Dióxido de nitrógeno Estratosfera info:eu-repo/semantics/conferenceObject 2015 ftaemet https://doi.org/20.500.11765/1137 2025-04-10T00:01:17Z Presentación realizada para el 7th International DOAS Workshop celebrado en Bruselas los días 6-8 de julio de 2015 Twenty years of stratospheric NO2 VCD data from ground-based zenith DOAS instruments have been used for trend analysis. Spectrometers either NDACC qualified or under evaluation cover Subtropical latitudes in Northern Hemisphere (Izaña, 28ºN), and Southern Antarctic (Marambio, 64ºS) and SubAntarctic (Ushuaia, 55ºS) regions. The multiple linear regression method includes annual, semiannual, quarterly, solar activity cycle, stratospheric aerosols, QBO and NAO proxies. The instruments settings follow the NDACC recommendations for NO2 measurements and the same AMF code. Results show a mean am/pm positive trend of + 7.9% at the 99% confidence level in the Northern Hemisphere station whereas the trends are negative in the Southern Hemisphere ones (-9.8% Ushuaia, -14.9% Marambio). From comparison with FTIR data, it is estimated that the changes are restricted to the lower stratosphere (15-30km) suggesting a dynamic origin of the trend. MIPAS NOy on a global scale shows a similar feature with a redistribution of the nitrogen family within the lower stratosphere. Conference Object Antarc* Antarctic ARCIMÍS (Archivo Climatológico y Meteorológico Institucional - AEMET, Agencia Estatal de Meteorología) Antarctic Marambio ENVELOPE(-56.750,-56.750,-64.283,-64.283) Ushuaia ENVELOPE(-40.000,-40.000,-82.167,-82.167)
spellingShingle Espectrómetros
Dióxido de nitrógeno
Estratosfera
Gil-Ojeda, Manuel
Yela González, Margarita
Navarro Comas, Mónica
Robles González, Cristina
Hase, F.
Funke, Bernd
Puentedura, Olga
Iglesias, Javier
Cuevas Agulló, Emilio
NO2 VCD Stratospheric trends Hemispheric and latitudinal dependence
title NO2 VCD Stratospheric trends Hemispheric and latitudinal dependence
title_full NO2 VCD Stratospheric trends Hemispheric and latitudinal dependence
title_fullStr NO2 VCD Stratospheric trends Hemispheric and latitudinal dependence
title_full_unstemmed NO2 VCD Stratospheric trends Hemispheric and latitudinal dependence
title_short NO2 VCD Stratospheric trends Hemispheric and latitudinal dependence
title_sort no2 vcd stratospheric trends hemispheric and latitudinal dependence
topic Espectrómetros
Dióxido de nitrógeno
Estratosfera
topic_facet Espectrómetros
Dióxido de nitrógeno
Estratosfera
url https://hdl.handle.net/20.500.11765/1137