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  • 1
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1997
    In:  Journal of Geophysical Research: Atmospheres Vol. 102, No. D11 ( 1997-06-20), p. 13141-13152
    In: Journal of Geophysical Research: Atmospheres, American Geophysical Union (AGU), Vol. 102, No. D11 ( 1997-06-20), p. 13141-13152
    Abstract: This paper focuses on the recovery of chlorine reservoir species in the lower stratosphere in late Antarctic spring. The investigations are based on measurements from the Halogen Occultation Experiment (HALOE) on board the Upper Atmosphere Research Satellite (UARS) and calculations by the Mainz photochemical box model and the NASA Langley Research Center trajectory model. During late Antarctic spring 1994, HALOE observed high HCl mixing ratios up to 2.7 ppbv at 20 km altitude in the ozone‐depleted air inside the polar vortex. These values correspond approximately to the sum of all available inorganic chlorine species. In the preceding period of chlorine activation on polar stratospheric clouds (PSCs), the observed HCl mixing ratios in some cases were below 0.3 ppbv. This indicates a fast conversion of active chlorine species into the form of HCl after PSCs disappear with increasing stratospheric temperatures. Box model calculations are presented that assess the rate of HCl increase in late spring when heterogeneous chemistry on polar stratospheric clouds becomes insignificant. The calculations were performed along Lagrangian trajectories starting from HALOE measurements in September 1994. Sensitivity calculations are presented regarding uncertainties in input parameters of the calculations. In the vortex edge region, calculated HCl increase rates are significantly lower compared with HALOE observations. Introducing additional HCl‐yielding branches of the reactions of ClO with OH and HO 2 helps to reduce this discrepancy.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1997
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  • 2
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2006
    In:  Journal of Geophysical Research Vol. 111, No. D24 ( 2006-12-20)
    In: Journal of Geophysical Research, American Geophysical Union (AGU), Vol. 111, No. D24 ( 2006-12-20)
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2006
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  • 3
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2009
    In:  Journal of Geophysical Research Vol. 114, No. D19 ( 2009-10-09)
    In: Journal of Geophysical Research, American Geophysical Union (AGU), Vol. 114, No. D19 ( 2009-10-09)
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2009
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  • 4
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1998
    In:  Journal of Geophysical Research: Atmospheres Vol. 103, No. D3 ( 1998-02-20), p. 3587-3597
    In: Journal of Geophysical Research: Atmospheres, American Geophysical Union (AGU), Vol. 103, No. D3 ( 1998-02-20), p. 3587-3597
    Abstract: Between May and September a continuous decrease of ozone concentrations is observed in the lower stratosphere at high latitudes in the northern hemisphere. Low local ozone concentrations are correlated with high concentrations of NO and NO 2 , and HCl. A detailed photochemical box model and a two‐dimensional chemical model initialized by the Halogen Occultation Experiment (HALOE) data are used to calculate ozone destruction rates between 20 and 31 km altitude for different situations during the observational periods in mid and late summer. The largest ozone destruction rates are computed for ozone‐rich midlatitude air masses that are transported to high latitudes reaching low Sun, but 24 hours per day sunlight conditions. It is shown that the observed summertime low ozone concentrations and much of the seasonal course of ozone is due to catalytic ozone destruction by NO and NO 2 , which become the main odd nitrogen compounds under these conditions.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1998
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  • 5
    In: Journal of Geophysical Research, American Geophysical Union (AGU), Vol. 111, No. D11 ( 2006)
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2006
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  • 6
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2003
    In:  Geophysical Research Letters Vol. 30, No. 23 ( 2003-12), p. n/a-n/a
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 30, No. 23 ( 2003-12), p. n/a-n/a
    Type of Medium: Online Resource
    ISSN: 0094-8276
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2003
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  • 7
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 24, No. 22 ( 1997-11-15), p. 2717-2720
    Type of Medium: Online Resource
    ISSN: 0094-8276
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1997
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  • 8
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1997
    In:  Journal of Geophysical Research: Atmospheres Vol. 102, No. D11 ( 1997-06-20), p. 13153-13167
    In: Journal of Geophysical Research: Atmospheres, American Geophysical Union (AGU), Vol. 102, No. D11 ( 1997-06-20), p. 13153-13167
    Abstract: The practicality of conducting photochemical calculations along trajectories of air masses is investigated. An isentropic trajectory package is used in conjunction with a detailed photochemical model to compare predictions of the mean chemical content of air masses initialized with the Halogen Occultation Experiment (HALOE) data with coincident in situ observations from instruments onboard the ER‐2 aircraft. Comparisons are made for 10 ER‐2 flights originating from Christchurch, New Zealand, during the May to June and October 1994 Airborne Southern Hemisphere Ozone Experiment/Measurements for Assessing the Effects of Stratospheric Aircraft (ASHOE/MAESA) deployments. Between 54 and 84 coincidences are found, depending on the species measured. Correlations between the ER‐2 and HALOE air mass/box model calculations are high (0.56–0.90) for most species considered except for H 2 O (0.14) and HCl (0.24). Statistically significant low biases in the prediction of HCl, H 2 O, and OH are found. Kolmogorov‐Smirnov (KS) significance tests are used to quantify the agreement between the distribution of species observed by the ER‐2 and predicted by the HALOE trajectory/ photochemical model. The model predictions agree with the observed variance within the distributions at significance levels greater than 0.80 (greater than 80% confidence that the predicted and observed variance are identical) for H 2 O, ClO, O 3 , and NO y . The impact of computational errors in the trajectory calculations and measurement uncertainty in the computed confidence levels are investigated using Monte Carlo techniques. Computational trajectory errors are found to play a small role in reducing confidence levels. The error analysis shows that the HALOE trajectory/photochemical model calculations reproduce the large‐scale variability found in the in situ ER‐2 constituent measurements to within the expected uncertainties in the HALOE observations for all species considered. It is concluded that the combined trajectory/photochemical model is an effective tool for interpreting in situ aircraft observations within the global perspective provided by remote satellite measurements.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1997
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  • 9
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2000
    In:  Journal of Geophysical Research: Atmospheres Vol. 105, No. D5 ( 2000-03-16), p. 6885-6890
    In: Journal of Geophysical Research: Atmospheres, American Geophysical Union (AGU), Vol. 105, No. D5 ( 2000-03-16), p. 6885-6890
    Abstract: Measurements have shown a substantial decrease in Northern midlatitude ozone, which has only partially been explained by chemical models. The large ozone depletions determined for the Arctic vortex in recent winters will ultimately spread out and dilute the midlatitudes and thus contribute to the observed decrease. Here we have followed the ozone‐depleted air inside the Arctic vortex in 1995 and 1997 during April and May with high‐resolution reverse domain‐filling (RDF) trajectory calculations. The resulting average midlatitude (30°–60°N) stratospheric ozone dilution in May is 2.9% and 2.6% of the 1979 column ozone in 1995 and 1997, respectively, or about 40% of the observed depletion. Nearly realistic mixing was introduced by a regridding procedure between successive 7‐day long RDF calculations. Low‐resolution grid point models give too much mixing, causing an overestimate of the calculated dilution. A recovery of about 12% of the midlatitude dilution in May 1997 is calculated with a photochemical box model, but is not included in the number given above.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2000
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  • 10
    In: Journal of Geophysical Research: Atmospheres, American Geophysical Union (AGU), Vol. 107, No. D5 ( 2002-03-16), p. SOL 45-1-SOL 45-17
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2002
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