Abstract

This paper presents the results of a statistical study of the spatiotemporal distribution of ozone in the upper troposphere and lower stratosphere (UTLS) regions induced by cut-off lows (COLs) over Northeast Asia. The analysis was based on high-resolution ERA-Interim ozone data and Atmospheric Infrared Sounder (AIRS) satellite data for the period from 2005–2015. A total of 186 COL events were detected. The observed ozone distribution revealed an ozone-rich region in the upper troposphere (300 hPa) located around the center of the COLs at the time when COLs reached their maximum intensity. This region corresponds to a region of high potential vorticity (PV). In the middle troposphere (500 hPa), enhanced levels of the ozone were distributed in two regions. The maximum concentration was located to the east of the COLs, and a secondary maximum region was in the center of the COLs. Further analysis revealed that this spatial distribution of ozone in the upper troposphere was affected mainly by decreased tropopause. The ozone was subject to a ‘rotary’ transport process in the middle troposphere, influenced mainly by the anticlockwise circulation of the COLs and the surrounding horizontal wind distribution. The temporal variations in ozone anomalies also revealed the ozone distribution patterns and transport processes. The variation in ozone anomalies implied that the magnitude of the ozone increase was closely related to the evolution of COLs lifecycle. The temporal and spatial distributions of the ozone revealed by the statistical analysis of the AIRS satellite data were overall consistent with those of the ERA-Interim data.

Highlights

  • Stratosphere–troposphere exchange (STE), which transports materials through the tropopause, is an important dynamic and chemical process that takes place in the region of the upper troposphere and lower stratosphere (UTLS)

  • This indicates that, during the development of cut-off lows (COLs), according to the Atmospheric Infrared Sounder (AIRS) satellite data, the distribution of the ozone in the middle troposphere was affected by the surrounding strong anticlockwise circulation of COLs, which is consistent with the results revealed in the previous section using ERA-Interim data

  • Cut-off low systems are synoptic-scale patterns that play an important role in STE in the extra-tropical UTLS region (Ex-UTLS)

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Summary

Introduction

Stratosphere–troposphere exchange (STE), which transports materials through the tropopause, is an important dynamic and chemical process that takes place in the region of the upper troposphere and lower stratosphere (UTLS). Model to simulate the STE process and found evidence of active exchange in a COL pre-formation stage These case studies have demonstrated that COLs play an important role in the redistribution of ozone in the Ex-UTLS region over Northeast Asia. In the present study, using high-resolution reanalysis data and Atmospheric Infrared Sounder (AIRS) satellite data, we examined COL events over Northeast Asia for the period of 2005–2015 and conducted a statistical analysis of the spatial distribution and temporal evolution of ozone in the UTLS region induced by COLs. The aim was to determine the effect of COLs on the ozone redistribution in the UTLS region.

Ozone and Meteorology Data
Methodology for Identifying Cut-Off Lows
Statistical Analysis of Cut-Off-Lows in Northeast Asia
The COLs Coordinates
The COLs Coordinate of ERA-Interim Dataset
Ozone Spatial Distribution Revealed by the ERA-Interim Dataset
Temporal Variations Revealed by the ERA-Interim Dataset
Temporal and Spatial Distributions Revealed by the AIRS Dataset
Findings
Summary and Discussion
Full Text
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