Strategies for measuring canonical tracer relationships in the stratosphere

Morgenstern, Olaf; Pyle, J. A.

doi:10.5194/acp-3-259-2003

Cited by 2 publications

(2 citation statements)

References 13 publications

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“…11a). The asymmetry of the midlatitude tracer-tracer correlation functions measured in both hemispheres is discussed in the literature (e.g., Morgenstern and Pyle, 2003).…”

Section: Tracer-tracer Relationships In the ∆χ N 2 O Parametrizationmentioning

confidence: 99%

A quasi-Lagrangian coordinate system based on high resolution tracer observations: implementation for the Antarctic polar vortex

Ivanova

Volk

Riediger

et al. 2008

Preprint

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Abstract. In order to quantitatively analyse the chemical and dynamical evolution of the polar vortex it has proven extremely useful to work with coordinate systems that follow the vortex flow. We propose here a two-dimensional quasi-Lagrangian coordinate system {χi, Δχi}, based on the mixing ratio of a long-lived stratospheric trace gas i, and its systematic use with i = N2O, in order to describe the structure of a well-developed Antarctic polar vortex. In the coordinate system {χi, Δχi} the mixing ratio χi is the vertical coordinate and Δχi = χi(Θ)−χivort(Θ) is the meridional coordinate (χivort(Θ) being a vertical reference profile in the vortex core). The quasi-Lagrangian coordinates {χi, Δχi} persist for much longer time than standard isentropic coordinates, potential temperature Θ and equivalent latitude φe, do not require explicit reference to geographic space, and can be derived directly from high-resolution in situ measurements. They are therefore well-suited for studying the evolution of the Antarctic polar vortex throughout the polar winter with respect to the relevant chemical and microphysical processes. By using the introduced coordinate system {χN2O, ΔχN2O} we analyze the well-developed Antarctic vortex investigated during the APE-GAIA (Airborne Polar Experiment – Geophysica Aircraft in Antarctica – 1999) campaign (Carli et al., 2000). A criterion, which uses the local in-situ measurements of χi=χi(Θ) and attributes the inner vortex edge to a rapid change (δ-step) in the meridional profile of the mixing ratio χi, is developed to determine the (Antarctic) inner vortex edge. In turn, we suggest that the outer vortex edge of a well-developed Antarctic vortex can be attributed to the position of a local minimum of the χH2O gradient in the polar vortex area. For a well-developed Antarctic vortex, the ΔχN2O-parametrization of tracer-tracer relationships allows to distinguish the tracer inter-relationships in the vortex core, vortex boundary region and surf zone and to examine their meridional variation throughout these regions. This is illustrated by analyzing the tracer-tracer relationships χi : χN2O obtained from the in-situ data of the APE-GAIA campaign for i = CFC-11, CFC-12, H-1211 and SF6. A number of solitary anomalous points in the CFC-11 : N2O correlation, observed in the Antarctic vortex core, are interpreted in terms of small-scale cross-isentropic dispersion.

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“…11a). The asymmetry of the midlatitude tracer-tracer correlation functions measured in both hemispheres is discussed in the literature (e.g., Morgenstern and Pyle, 2003).…”

Section: Tracer-tracer Relationships In the ∆χ N 2 O Parametrizationmentioning

confidence: 99%

A quasi-Lagrangian coordinate system based on high resolution tracer observations: implementation for the Antarctic polar vortex

Ivanova

Volk

Riediger

et al. 2008

Preprint

View full text Add to dashboard Cite

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“…The uncertainties and footprint of HALOE data are larger than for in situ data. Morgenstern and Pyle (2003) assessed the effects of these factors on the ability to distinguish different tracer correlations across the stratospheric polar vortex. They concluded that although HALOE might be inappropriate for localized studies, for low-resolution studies the redundancy in the data should allow the accurate differentiation of tracer correlations.…”

Section: The Haloe Datasetmentioning

confidence: 99%

An entropy-based measure of mixing at the tropopause

Patmore

Toumi

2006

Q.J.R. Meteorol. Soc.

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SUMMARYQualitative analysis of tracer correlations is now a well established technique for investigating mixing in the tropopause transition layer. Generally, these studies rely on in situ data retrieved over short distances and time-scales. Using satellite data from HALOE, we introduce a simple quantitative analysis technique, based on entropy, to provide a climatology of mixing, from H 2 O:O 3 tracer correlations. Results compare well with previous studies using Lagrangian-based estimates of effective diffusivity and equivalent lengths and also climatologies of tropopause folding. Further analysis techniques reveal characteristics of the transition layer, including its depth and position, leading to the distinction of three primary forms of mixing. Within our analysis domain, we estimate that half of total entropy can be attributed to subtropical 'Rossby-driven' tropopause folding events. The majority of the remaining entropy is associated with tropical convective mixing and a third form, possibly linked to shearinduced mixing at subtropical jet streaks.

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Strategies for measuring canonical tracer relationships in the stratosphere

Cited by 2 publications

References 13 publications

A quasi-Lagrangian coordinate system based on high resolution tracer observations: implementation for the Antarctic polar vortex

A quasi-Lagrangian coordinate system based on high resolution tracer observations: implementation for the Antarctic polar vortex

An entropy-based measure of mixing at the tropopause

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