Commentary on using equivalent latitude in the upper troposphere and lower stratosphere

We discuss the use of potential vorticity (PV) based equivalent latitude (EqLat) and potential temperature (<i>θ</i>) coordinates in the upper troposphere and lower stratosphere (UTLS) for chemical transport studies. The main objective is to provide a cautio...

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Bibliographic Details
Main Authors: L. L. Pan, A. Kunz, C. R. Homeyer, L. A. Munchak, D. E. Kinnison, S. Tilmes
Format: Article
Language:English
Published: Copernicus Publications 2012-10-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/12/9187/2012/acp-12-9187-2012.pdf
Description
Summary:We discuss the use of potential vorticity (PV) based equivalent latitude (EqLat) and potential temperature (<i>θ</i>) coordinates in the upper troposphere and lower stratosphere (UTLS) for chemical transport studies. The main objective is to provide a cautionary note on using EqLat-<i>θ</i> coordinates for aggregating chemical tracers in the UTLS. Several examples are used to show 3-D distributions of EqLat together with chemical constituents for a range of <i>θ</i>. We show that the use of PV-<i>θ</i> coordinates may not be suitable for several reasons when tropospheric processes are an important part of a study. Due to the different static stability structures between the stratosphere and troposphere, the use of <i>θ</i> as a vertical coordinate does not provide equal representations of the UT and LS. Since the <i>θ</i> surfaces in the troposphere often intersect the surface of the Earth, the <i>θ</i> variable does not work well distinguishing the UT from the boundary layer when used globally as a vertical coordinate. We further discuss the duality of PV/EqLat as a tracer versus as a coordinate variable. Using an example, we show that while PV/EqLat serves well as a transport tracer in the UTLS region, it may conceal the chemical structure associated with wave breaking when used as a coordinate to average chemical tracers. Overall, when choosing these coordinates, considerations need to be made not only based on the time scale of PV being a conservative tracer, but also the specific research questions to be addressed.
ISSN:1680-7316
1680-7324