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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ftaemet:oai:repositorio.aemet.es:20.500.11765/1137 2024-06-23T07:47:20+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 2024-06-03T14:17:56Z 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) |
institution |
Open Polar |
collection |
ARCIMÍS (Archivo Climatológico y Meteorológico Institucional - AEMET, Agencia Estatal de Meteorología) |
op_collection_id |
ftaemet |
language |
English |
topic |
Espectrómetros Dióxido de nitrógeno Estratosfera |
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 |
topic_facet |
Espectrómetros Dióxido de nitrógeno Estratosfera |
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. |
format |
Conference Object |
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 |
title |
NO2 VCD Stratospheric trends Hemispheric and latitudinal dependence |
title_short |
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_sort |
no2 vcd stratospheric trends hemispheric and latitudinal dependence |
publishDate |
2015 |
url |
https://hdl.handle.net/20.500.11765/1137 |
long_lat |
ENVELOPE(-56.750,-56.750,-64.283,-64.283) ENVELOPE(-40.000,-40.000,-82.167,-82.167) |
geographic |
Antarctic Marambio Ushuaia |
geographic_facet |
Antarctic Marambio Ushuaia |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_relation |
http://hdl.handle.net/20.500.11765/1137 |
op_rights |
Licencia CC: Reconocimiento–NoComercial–SinObraDerivada CC BY-NC-ND info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/20.500.11765/1137 |
_version_ |
1802651418906066944 |