In situ measurement of H2O and CH4 with telecommunication laser diodes in the lower stratosphere: Dehydration and indication of a tropical air intrusion at mid-latitudes
Telecommunication laser diodes emitting near 1.39 μ m and 1.65 μ m in combination with direct-differential absorption spectroscopy are efficient tools to monitor in situ stratospheric H^sub 2^O andCH^sub 4^ with a good precision error (a few percents), a high temporal resolution (ranging from 10 ms...
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Veröffentlicht in: | Journal of atmospheric chemistry 2002-11, Vol.43 (3), p.175-194 |
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creator | DURRY, Georges HAUCHECORNE, Alain OVARLEZ, Joelle OVARLEZ, Henri POUCHET, Ivan ZENINARI, Virginie PARVITTE, Bertrand |
description | Telecommunication laser diodes emitting near 1.39 μ m and 1.65 μ m in combination with direct-differential absorption spectroscopy are efficient tools to monitor in situ stratospheric H^sub 2^O andCH^sub 4^ with a good precision error (a few percents), a high temporal resolution (ranging from 10 ms to 1 s), a large dynamic range in the concentration measurements (four orders of magnitude) and a high selectivity in the analyte species. To illustrate the capability of laser probing technique, we report balloonborne H^sub 2^Oand CH^sub 4^ simultaneous measurements obtained on October 2001 atmidlatitudes (43° N). The H^sub 2^O vertical profile achieved with the lasersensor in the lower stratosphere is compared with the H^sub 2^O data yielded by a balloonborne frost-point hygrometer. The total hydrogen mixing ratio in the lower stratosphere, 2[CH^sub 4^] + [H^sub 2^O], appears to beconstant at 7.5 ± 0.1 ppmv. Nevertheless, an unexpected largedehydration of 0.5 ppmv was detected by both the laser sensor and thehygrometer between 16 km and 23 km. We suspect the occurrence of a tropicalair intrusion into mid-latitudes. We support this interpretation using a high-resolution advection model for potential vorticity.[PUBLICATION ABSTRACT] |
doi_str_mv | 10.1023/A:1020674208207 |
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To illustrate the capability of laser probing technique, we report balloonborne H^sub 2^Oand CH^sub 4^ simultaneous measurements obtained on October 2001 atmidlatitudes (43° N). The H^sub 2^O vertical profile achieved with the lasersensor in the lower stratosphere is compared with the H^sub 2^O data yielded by a balloonborne frost-point hygrometer. The total hydrogen mixing ratio in the lower stratosphere, 2[CH^sub 4^] + [H^sub 2^O], appears to beconstant at 7.5 ± 0.1 ppmv. Nevertheless, an unexpected largedehydration of 0.5 ppmv was detected by both the laser sensor and thehygrometer between 16 km and 23 km. We suspect the occurrence of a tropicalair intrusion into mid-latitudes. We support this interpretation using a high-resolution advection model for potential vorticity.[PUBLICATION ABSTRACT]</description><identifier>ISSN: 0167-7764</identifier><identifier>EISSN: 1573-0662</identifier><identifier>DOI: 10.1023/A:1020674208207</identifier><identifier>CODEN: JATCE2</identifier><language>eng</language><publisher>Dordrecht: Springer</publisher><subject>Absorption spectroscopy ; Atmospheric and Oceanic Physics ; Atmospheric composition. 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To illustrate the capability of laser probing technique, we report balloonborne H^sub 2^Oand CH^sub 4^ simultaneous measurements obtained on October 2001 atmidlatitudes (43° N). The H^sub 2^O vertical profile achieved with the lasersensor in the lower stratosphere is compared with the H^sub 2^O data yielded by a balloonborne frost-point hygrometer. The total hydrogen mixing ratio in the lower stratosphere, 2[CH^sub 4^] + [H^sub 2^O], appears to beconstant at 7.5 ± 0.1 ppmv. Nevertheless, an unexpected largedehydration of 0.5 ppmv was detected by both the laser sensor and thehygrometer between 16 km and 23 km. We suspect the occurrence of a tropicalair intrusion into mid-latitudes. We support this interpretation using a high-resolution advection model for potential vorticity.[PUBLICATION ABSTRACT]</description><subject>Absorption spectroscopy</subject><subject>Atmospheric and Oceanic Physics</subject><subject>Atmospheric composition. 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To illustrate the capability of laser probing technique, we report balloonborne H^sub 2^Oand CH^sub 4^ simultaneous measurements obtained on October 2001 atmidlatitudes (43° N). The H^sub 2^O vertical profile achieved with the lasersensor in the lower stratosphere is compared with the H^sub 2^O data yielded by a balloonborne frost-point hygrometer. The total hydrogen mixing ratio in the lower stratosphere, 2[CH^sub 4^] + [H^sub 2^O], appears to beconstant at 7.5 ± 0.1 ppmv. Nevertheless, an unexpected largedehydration of 0.5 ppmv was detected by both the laser sensor and thehygrometer between 16 km and 23 km. We suspect the occurrence of a tropicalair intrusion into mid-latitudes. 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subjects | Absorption spectroscopy Atmospheric and Oceanic Physics Atmospheric composition. Chemical and photochemical reactions Dehydration Earth, ocean, space Exact sciences and technology External geophysics In situ measurement Ozone Physics Physics of the high neutral atmosphere Stratosphere |
title | In situ measurement of H2O and CH4 with telecommunication laser diodes in the lower stratosphere: Dehydration and indication of a tropical air intrusion at mid-latitudes |
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