UNIDEF   23986
UNIDAD DE INVESTIGACION Y DESARROLLO ESTRATEGICO PARA LA DEFENSA
Unidad Ejecutora - UE
congresos y reuniones científicas
Título:
Systematic Ozone and Solar UV Measurements in the Observatorio Atmosférico de la Patagonia Austral, Argentina
Autor/es:
WOLFRAM, E., SALVADOR, J., ORTE, F, DELIA, R., ZAMORANO, F.,CASICCIA, C., PAES LEME, N., QUEL
Lugar:
La Paz
Reunión:
Workshop; 6 Workshop of Lidar Measureement in latin America; 2011
Resumen:
The depletion of the polar ozone layer is one of the
strongest anthropogenic signals in the Earth system. Subpolar regions in the
southern part of South America are affected by this phenomenon, covered
sometimes by air masses with less ozone than normal with the corresponding UV
enhancements at ground surface. Motivated by these atmospheric events, Argentina and Chile with the financial support of
JICA has joined scientific efforts to develop UVO3 Patagonia
project. It has as main objectives monitoring ozone and UV radiation in
Southern Patagonia. The Ozone and RUV laboratory (Chile) and the Lidar
Division of CEILAP (Argentina) are the execute laboratories of this project.
The Observatorio
Atmosférico de la Patagonia Austral (Atmospheric Observatory of Southern Patagonia) is
located in South Patagonia (51º 55S, 69º 14W), in subpolar region and it is a convenient
monitoring site of the atmosphere in the Southern Hemisphere. In this
experimental site is operative a differential absorption lidar instrument
(DIAL) for the measurement of ozone vertical distribution. This instrument
belongs of Network Data for Atmospheric Composition Change (NDACC). The
altitude range of the ozone measurement is 14-45 km, which provides the
opportunity to monitor the perturbations due to the passage of stratospheric
polar air over Río Gallegos. Systematic stratospheric ozone profile
measurement has been carried on in this experimental site since 2005. We
identified three mayor perturbation of ozone hole over the stratospheric
ozone profile in Río Gallegos. Approach of polar vortex during late winter,
overpass of ozone hole in middle spring and dilution process during late
spring change the shape and content of stratospheric ozone profile and by
consequences the solar UV. Solar surface irradiance and total ozone content
were measured with a Brewer spectraphotometer and moderate narrow band
radiometer GUV-541 deployed in the Río Gallegos experimental site.
Depleted ozone columns were measured
during ozone hole overpass, and the analysis of unique extreme ozone
depletion event in November 2009 is reported and compared with Multisensor
Data Reanalysis of TOMS/OMI satellite data.