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- W4247249609 abstract "Abstract. The Superconducting Submillimeter-Wave Limb-Emission Sounder (SMILES) on board the International Space Station observed ozone profiles in the stratosphere with high sensitivity. Although SMILES measurements do not cover high latitudes, the combination of data assimilation methods and an isentropic advection model allows us to use SMILES measurements to investigate the ozone loss due to the instability of the polar vortex in the northern hemisphere. We quantified the ozone depletion in the 2009/2010 Arctic polar winter. Ozone data from both SMILES and Odin/SMR (Sub-Millimetre Radiometer) for the winter were assimilated into the Dynamical Isentropic Assimilation Model for OdiN Data (DIAMOND). DIAMOND is an off-line wind-driven transport model on isentropic surfaces. Wind data from the European Centre for Medium-Range Weather Forecasts (ECMWF) were used to drive the model. In this study, particular attention is paid to the cross isentropic transport of the tracer. The assimilated SMILES ozone fields agree with the SMR fields despite the limited latitude coverage. Ozone depletion has been derived by comparing the ozone field acquired by sequential assimilation with a passively transported ozone field initiated to 1 December 2009. Significant ozone loss was found in different periods and altitudes from using both SMILES and SMR data. The initial depletion occurred in the end of January below 500 K with a loss of 0.6–1.0 ppm (approximately 20%). The ensuing loss started from the end of February between 575 K and 650 K. Our estimation shows that 0.8 ppmv (15–20%) of O3 has been removed from the lower stratosphere by 1 April in VMR." @default.
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- W4247249609 date "2014-03-24" @default.
- W4247249609 modified "2023-09-29" @default.
- W4247249609 title "The use of SMILES data to study ozone loss in the Arctic winter 2009/2010 and comparison with Odin/SMR data using assimilation techniques" @default.
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- W4247249609 doi "https://doi.org/10.5194/acpd-14-7889-2014" @default.
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