http://www.cnr.it/ontology/cnr/individuo/prodotto/ID191732
Extreme ozone depletion in the 2010-2011 Arctic winter stratosphere as observed by MIPAS/ENVISAT using a 2-D tomographic approach (Articolo in rivista)
- Type
- Label
- Extreme ozone depletion in the 2010-2011 Arctic winter stratosphere as observed by MIPAS/ENVISAT using a 2-D tomographic approach (Articolo in rivista) (literal)
- Anno
- 2012-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.5194/acp-12-9149-2012 (literal)
- Alternative label
E. Arnone1, E. Castelli, E. Papandrea, M. Carlotti, and B. M. Dinelli (2012)
Extreme ozone depletion in the 2010-2011 Arctic winter stratosphere as observed by MIPAS/ENVISAT using a 2-D tomographic approach
in Atmospheric chemistry and physics (Online); Copernicus Publications, Göttingen (Germania)
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- E. Arnone1, E. Castelli, E. Papandrea, M. Carlotti, and B. M. Dinelli (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- 1 IIstituto di Scienza dell'Atmosfera e del Clima - CNR, Bologna, Italy
2 Dipartimento di Chimica Fisica e Inorganica, Università di Bologna, Bologna, Italy (literal)
- Titolo
- Extreme ozone depletion in the 2010-2011 Arctic winter stratosphere as observed by MIPAS/ENVISAT using a 2-D tomographic approach (literal)
- Abstract
- We present observations of the 2010-2011 Arc-
tic winter stratosphere from the Michelson Interferometer for
Passive Atmospheric Sounding (MIPAS) onboard ENVISAT.
Limb sounding infrared measurements were taken by MIPAS
during the Northern polar winter and into the subsequent
spring, giving a continuous vertically resolved view of the
Arctic dynamics, chemistry and polar stratospheric clouds
(PSCs). We adopted a 2-D tomographic retrieval approach
to account for the strong horizontal inhomogeneity of the at-
mosphere present under vortex conditions, self-consistently
comparing 2011 to the 2-D analysis of 2003-2010. Unlike
most Arctic winters, 2011 was characterized by a strong
stratospheric vortex lasting until early April. Lower strato-
spheric temperatures persistently remained below the thresh-
old for PSC formation, extending the PSC season up to mid-
March, resulting in significant chlorine activation leading to
ozone destruction. On 3 January 2011, PSCs were detected
up to 30.5 ± 0.9 km altitude, representing the highest PSCs
ever reported in the Arctic. Through inspection of MIPAS
spectra, 83 % of PSCs were identified as supercooled ternary
solution (STS) or STS mixed with nitric acid trihydrate
(NAT), 17 % formed mostly by NAT particles, and only two
cases by ice. In the lower stratosphere at potential tempera-
ture 450 K, vortex average ozone showed a daily depletion
rate reaching 100 ppbv day-1 . In early April at 18 km alti-
tude, 10 % of vortex measurements displayed total depletion
of ozone, and vortex average values dropped to 0.6 ppmv.
This corresponds to a chemical loss from early winter greater
than 80 %. Ozone loss was accompanied by activation of
ClO, associated depletion of its reservoir ClONO2 , and sig-
nificant denitrification, which further delayed the recovery
of ozone in spring. Once the PSC season halted, ClO was re-
converted primarily into ClONO2 . Compared to MIPAS ob-
served 2003-2010 Arctic average values, the 2010-2011 vor-
tex in late winter had 15 K lower temperatures, 40 % lower
HNO3 and 50 % lower ozone, reaching the largest ozone de-
pletion ever observed in the Arctic. The overall picture of this
Arctic winter was remarkably closer to conditions typically
found in the Antarctic vortex than ever observed before. (literal)
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