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Fractional release factors of long-lived halogenated organic compounds in the tropical stratosphere

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TLDR
In this paper, the first set of vertically resolved fractional release factors for 15 long-lived halocarbons in the tropical stratosphere up to 34 km altitude were calculated from measurements on air samples collected on board balloons and a high altitude aircraft.
Abstract
Fractional release factors (FRFs) of organic trace gases are time-independent quantities that influence the calculation of Global Warming Potentials and Ozone Depletion Potentials. We present the first set of vertically resolved FRFs for 15 long-lived halocarbons in the tropical stratosphere up to 34 km altitude. They were calculated from measurements on air samples collected on board balloons and a high altitude aircraft. We compare the derived dependencies of FRFs on the mean stratospheric transit times (the so-called mean ages of air) with similarly derived FRFs originating from measurements at higher latitudes and find significant differences. Moreover a comparison with averaged FRFs currently used by the World Meteorological Organisation revealed the limitations of these measures due to their observed vertical and latitudinal variability. The presented data set could be used to improve future ozone level and climate projections.

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Reconciliation of essential process parameters for an enhanced predictability of Arctic stratospheric ozone loss and its climate interactions (RECONCILE): activities and results

M. von Hobe, +93 more
TL;DR: The European project RECONCILE has comprehensively addressed remaining questions in the context of polar ozone depletion, with the objective to quantify the rates of some of the most relevant, yet still uncertain physical and chemical processes as mentioned in this paper.
Journal ArticleDOI

A review of major chlorofluorocarbons and their halocarbon alternatives in the air

TL;DR: In this article, the authors provide an overview of the global chemistry of CFCs and their alternatives, their production and emission trends, their relationship with the ozone depletion phenomenon, the chemistry regulating their removal processes, and their distribution patterns with diverse temporal and spatial scales.
Journal ArticleDOI

Observation-based assessment of stratospheric fractional release, lifetimes, and ozone depletion potentials of ten important source gases

TL;DR: In this article, the authors present data from the analysis of air samples collected between 2009 and 2011 on board research aircraft flying in the mid and high-latitude stratosphere and infer the above-mentioned parameters for ten major source gases: CFCl3 (CFC-11), CF2Cl2 (cFC-12),CF2ClCFCl2(cfc-113), CCl4 (carbon tetrachloride), CH3CCl3(methyl chloroform), CHF2Cl (HCFC-22, CH3CFClCl
References
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Journal ArticleDOI

Chlorofluoromethanes in the Environment

TL;DR: In this article, the photoprocesses of atmospheric chlorofluoromethanes, including their ultimate sinks, are studied. Butt et al. present a detailed study of the photodissociation process of chlorofluromethane.
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Age as a diagnostic of stratospheric transport

TL;DR: In this paper, the authors employ a one-dimensional diffusive analog of stratospheric transport, and the general circulation model (GCM) of the Goddard Institute for Space Studies (GISS), to estimate the time over which tropospheric tracer concentrations must be approximately linear in order to determine stratosphere age unambiguously, if the growth time constant is greater than about 7 years.
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Age of stratospheric air: theory, observations, and models

TL;DR: The relationship between tracer distributions and transport timescales in the stratosphere is discussed in this article, where the authors use the age spectrum, the distribution of transit times since stratospheric air last made tropospheric contact, to understand the transport information of tracers, how sensitive different tracers are to various transport processes and how to use tracers in combination to constrain transport rates.
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Interrelationships between mixing ratios of long‐lived stratospheric constituents

TL;DR: In this article, a 2D chemistry-transport model was used to show that species with longer lifetimes than vertical transport time scales are in gradient equilibrium and their mixing ratios display a linear relationship.
Journal ArticleDOI

A “tropical pipe” model of stratospheric transport

TL;DR: In this article, a conceptual model of global stratospheric transport is described, based on the assumption of rapid isentropic mixing within midlatitude "surf zones" but weak mixing into the tropics.
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