Capitulo de libro
STRATOSPHERIC OZONE MONITORING OVER NY ALESUND
Fecha
2013Institución
Resumen
The paper shows some results of campaigns performed at the “Dirigibile Italia“ Station,
useful for comparing satellite and ground-based stratospheric ozone concentrations, both
acquired during the polar day, and analyzing the results of ozone measurements during
a polar winter campaign using a special routine to evaluate the O3
with UV radiation
reflected by the Moon. The work is completed with a particular fast measurement during
the eclipse event of Aug. 1st, 2008.The paper shows some results of campaigns performed at the “Dirigibile Italia“ Station,
useful for comparing satellite and ground-based stratospheric ozone concentrations, both
acquired during the polar day, and analyzing the results of ozone measurements during
a polar winter campaign using a special routine to evaluate the O3
with UV radiation
reflected by the Moon. The work is completed with a particular fast measurement during
the eclipse event of Aug. 1st, 2008.The paper shows some results of campaigns performed at the “Dirigibile Italia“ Station,
useful for comparing satellite and ground-based stratospheric ozone concentrations, both
acquired during the polar day, and analyzing the results of ozone measurements during
a polar winter campaign using a special routine to evaluate the O3
with UV radiation
reflected by the Moon. The work is completed with a particular fast measurement during
the eclipse event of Aug. 1st, 2008.The paper shows some results of campaigns performed at the “Dirigibile Italia“ Station,
useful for comparing satellite and ground-based stratospheric ozone concentrations, both
acquired during the polar day, and analyzing the results of ozone measurements during
a polar winter campaign using a special routine to evaluate the O3
with UV radiation
reflected by the Moon. The work is completed with a particular fast measurement during
the eclipse event of Aug. 1st, 2008.The paper shows some results of campaigns performed at the “Dirigibile Italia“ Station,
useful for comparing satellite and ground-based stratospheric ozone concentrations, both
acquired during the polar day, and analyzing the results of ozone measurements during
a polar winter campaign using a special routine to evaluate the O3
with UV radiation
reflected by the Moon. The work is completed with a particular fast measurement during
the eclipse event of Aug. 1st, 2008.The paper shows some results of campaigns performed at the “Dirigibile Italia“ Station,
useful for comparing satellite and ground-based stratospheric ozone concentrations, both
acquired during the polar day, and analyzing the results of ozone measurements during
a polar winter campaign using a special routine to evaluate the O3
with UV radiation
reflected by the Moon. The work is completed with a particular fast measurement during
the eclipse event of Aug. 1st, 2008.The paper shows some results of campaigns performed at the “Dirigibile Italia“ Station,
useful for comparing satellite and ground-based stratospheric ozone concentrations, both
acquired during the polar day, and analyzing the results of ozone measurements during
a polar winter campaign using a special routine to evaluate the O3
with UV radiation
reflected by the Moon. The work is completed with a particular fast measurement during
the eclipse event of Aug. 1st, 2008.The paper shows some results of campaigns performed at the “Dirigibile Italia“ Station,
useful for comparing satellite and ground-based stratospheric ozone concentrations, both
acquired during the polar day, and analyzing the results of ozone measurements during
a polar winter campaign using a special routine to evaluate the O3
with UV radiation
reflected by the Moon. The work is completed with a particular fast measurement during
the eclipse event of Aug. 1st, 2008.The paper shows some results of campaigns performed at the “Dirigibile Italia“ Station,
useful for comparing satellite and ground-based stratospheric ozone concentrations, both
acquired during the polar day, and analyzing the results of ozone measurements during
a polar winter campaign using a special routine to evaluate the O3
with UV radiation
reflected by the Moon. The work is completed with a particular fast measurement during
the eclipse event of Aug. 1st, 2008.The paper shows some results of campaigns performed at the “Dirigibile Italia“ Station,
useful for comparing satellite and ground-based stratospheric ozone concentrations, both
acquired during the polar day, and analyzing the results of ozone measurements during
a polar winter campaign using a special routine to evaluate the O3
with UV radiation
reflected by the Moon. The work is completed with a particular fast measurement during
the eclipse event of Aug. 1st, 2008.The paper shows some results of campaigns performed at the “Dirigibile Italia“ Station,
useful for comparing satellite and ground-based stratospheric ozone concentrations, both
acquired during the polar day, and analyzing the results of ozone measurements during
a polar winter campaign using a special routine to evaluate the O3
with UV radiation
reflected by the Moon. The work is completed with a particular fast measurement during
the eclipse event of Aug. 1st, 2008.The paper shows some results of campaigns performed at the “Dirigibile Italia“ Station,
useful for comparing satellite and ground-based stratospheric ozone concentrations, both
acquired during the polar day, and analyzing the results of ozone measurements during
a polar winter campaign using a special routine to evaluate the O3
with UV radiation
reflected by the Moon. The work is completed with a particular fast measurement during
the eclipse event of Aug. 1st, 2008.The paper shows some results of campaigns performed at the “Dirigibile Italia“ Station,
useful for comparing satellite and ground-based stratospheric ozone concentrations, both
acquired during the polar day, and analyzing the results of ozone measurements during
a polar winter campaign using a special routine to evaluate the O3
with UV radiation
reflected by the Moon. The work is completed with a particular fast measurement during
the eclipse event of Aug. 1st, 2008.