Millimeter wave spectroscopic measurements of stratospheric and mesospheric constituents over the Italian Alps: stratospheric ozone

Measurements of rotational lines emitted by middle atmospheric trace gases have been carried out from the Alpine station of Testa Grigia (45.9°N, 7.7°E, elev. 3500 m) by means of a Ground-Based Millimeter-wave Spectrometer (GBMS). Observations of species such as O3, HNO3, CO, N2O, HCN, and HDO took...

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Published in:Journal of Geophysical Research: Atmospheres
Main Authors: Muscari, G., Cesaroni, C., Bianchi, C., de Zafra, R. L., Di Iorio, T., Fiorucci, I., Fuà, D., Romaniello, V., Zuccheretti, E.
Other Authors: Muscari, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia, Cesaroni, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia, Bianchi, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia, de Zafra, R. L.; Department of Physics and Astronomy and Institute for Terrestrial and Planetary Atmospheres, Di Iorio, T.; Dipartimento di Fisica, Università degli Studi di Roma «La Sapienza», Roma, Italy, Fiorucci, I.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia, Fuà, D.; Dipartimento di Fisica, Università degli Studi di Roma «La Sapienza», Roma, Italy, Romaniello, V.; Dipartimento di Fisica, Università degli Studi di Roma «La Sapienza», Roma, Italy, Zuccheretti, E.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia, Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia, Department of Physics and Astronomy and Institute for Terrestrial and Planetary Atmospheres, Dipartimento di Fisica, Università degli Studi di Roma «La Sapienza», Roma, Italy
Format: Article in Journal/Newspaper
Language:English
Published: Editrice Compositori 2007
Subjects:
Online Access:http://hdl.handle.net/2122/3678
id ftingv:oai:www.earth-prints.org:2122/3678
record_format openpolar
institution Open Polar
collection Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia)
op_collection_id ftingv
language English
topic millimeter-wave spectroscopy
stratospheric ozone
isentropic transport
01. Atmosphere::01.01. Atmosphere::01.01.99. General or miscellaneous
spellingShingle millimeter-wave spectroscopy
stratospheric ozone
isentropic transport
01. Atmosphere::01.01. Atmosphere::01.01.99. General or miscellaneous
Muscari, G.
Cesaroni, C.
Bianchi, C.
de Zafra, R. L.
Di Iorio, T.
Fiorucci, I.
Fuà, D.
Romaniello, V.
Zuccheretti, E.
Millimeter wave spectroscopic measurements of stratospheric and mesospheric constituents over the Italian Alps: stratospheric ozone
topic_facet millimeter-wave spectroscopy
stratospheric ozone
isentropic transport
01. Atmosphere::01.01. Atmosphere::01.01.99. General or miscellaneous
description Measurements of rotational lines emitted by middle atmospheric trace gases have been carried out from the Alpine station of Testa Grigia (45.9°N, 7.7°E, elev. 3500 m) by means of a Ground-Based Millimeter-wave Spectrometer (GBMS). Observations of species such as O3, HNO3, CO, N2O, HCN, and HDO took place during 4 winter periods, from February 2004 to March 2007, for a total of 116 days of measurements grouped in about 18 field campaigns. By studying the pressure-broadened shape of emission lines the vertical distribution of the observed constituents is retrieved within an altitude range of ∼17-75 km, constrained by the 600 MHz pass band and the 65 kHz spectral resolution of the back-end spectrometer. This work discusses the behavior of stratospheric O3 during the entire period of operation at Testa Grigia. Mid-latitude O3 columnar content as estimated using GBMS measurements can vary by large amounts over a period of very few days, with the largest variations observed in December 2005, February 2006, and March 2006, confirming that the northern winter of 2005-2006 was characterized by a particularly intense planetary wave activity. The largest rapid variation from maximum to minimum O3 column values over Testa Grigia took place in December 2006 and reached a relative value of 72% with respect to the average column content for that period. During most GBMS observation times much of the variability is concentrated in the column below 20 km, with tropospheric weather systems and advection of tropical tropospheric air into the lower stratosphere over Testa Grigia having a large impact on the observed variations in column contents. Nonetheless, a wide variability is also found in middle stratospheric GBMS O3 measurements, as expected for mid-latitude ozone. We find that O3 mixing ratios at ∼32 km are very well correlated with the solar illumination experienced by air masses over the previous ∼15 days, showing that already at 32 km altitude ozone photochemistry dominates over transport processes. The correlation of ...
author2 Muscari, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia
Cesaroni, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia
Bianchi, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia
de Zafra, R. L.; Department of Physics and Astronomy and Institute for Terrestrial and Planetary Atmospheres,
Di Iorio, T.; Dipartimento di Fisica, Università degli Studi di Roma «La Sapienza», Roma, Italy
Fiorucci, I.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia
Fuà, D.; Dipartimento di Fisica, Università degli Studi di Roma «La Sapienza», Roma, Italy
Romaniello, V.; Dipartimento di Fisica, Università degli Studi di Roma «La Sapienza», Roma, Italy
Zuccheretti, E.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia
Department of Physics and Astronomy and Institute for Terrestrial and Planetary Atmospheres,
Dipartimento di Fisica, Università degli Studi di Roma «La Sapienza», Roma, Italy
format Article in Journal/Newspaper
author Muscari, G.
Cesaroni, C.
Bianchi, C.
de Zafra, R. L.
Di Iorio, T.
Fiorucci, I.
Fuà, D.
Romaniello, V.
Zuccheretti, E.
author_facet Muscari, G.
Cesaroni, C.
Bianchi, C.
de Zafra, R. L.
Di Iorio, T.
Fiorucci, I.
Fuà, D.
Romaniello, V.
Zuccheretti, E.
author_sort Muscari, G.
title Millimeter wave spectroscopic measurements of stratospheric and mesospheric constituents over the Italian Alps: stratospheric ozone
title_short Millimeter wave spectroscopic measurements of stratospheric and mesospheric constituents over the Italian Alps: stratospheric ozone
title_full Millimeter wave spectroscopic measurements of stratospheric and mesospheric constituents over the Italian Alps: stratospheric ozone
title_fullStr Millimeter wave spectroscopic measurements of stratospheric and mesospheric constituents over the Italian Alps: stratospheric ozone
title_full_unstemmed Millimeter wave spectroscopic measurements of stratospheric and mesospheric constituents over the Italian Alps: stratospheric ozone
title_sort millimeter wave spectroscopic measurements of stratospheric and mesospheric constituents over the italian alps: stratospheric ozone
publisher Editrice Compositori
publishDate 2007
url http://hdl.handle.net/2122/3678
genre Arctic
genre_facet Arctic
op_relation Annals of Geophysics
3/50 (2007)
BRAATHEN, G. (2006): Joint WMO/EU Arctic Ozone Bulletin, Winter/Spring Summary (World Meteorological Organization/European Ozone Research Coordinating Unit), Tech. Rep. 2006-1 (available on line at: <http://www.wmo.int/pages/prog/arep/gaw/ozone/in dex.html>). CHENG, D., R.L. DE ZAFRA and C. TRIMBLE (1996): Millimeter wave spectroscopic measurements over the South Pole, 2. An 11-month cycle of stratospheric ozone observations during 1993-1994, J. Geophys. Res., 101, 6781- 6793. DE ZAFRA, R.L. (1995): The ground-based measurements of stratospheric trace gases using quantitative millimeter wave emission spectroscopy, in ‘Diagnostic Tools in Atmospheric Physics’, Proceedings of the International School of Physics «Enrico Fermi», edited by G. FIOCCO and G. VISCONTI (Elsevier, New York), 124, 23-54. DE ZAFRA, R.L. and G. MUSCARI (2004): CO as an important high-altitude tracer of dynamics in the polar stratosphere and mesosphere, J. Geophys. Res., 109 (D06105), doi:10.1029/2003JD004099. DE ZAFRA, R. L.,V. CHAN, S. CREWELL, C. TRIMBLE and J.M. REEVES (1997): Millimeter wave spectroscopic measurements over the South Pole, 3. The behavior of stratospheric nitric acid through polar fall, winter, and spring, J. Geophys. Res., 102, 1399-1410. DOBSON, G.M.B., D.N. HARRISON and J. LAWRENCE (1929): Measurements of the amount of ozone in the earth’s atmosphere and its relation to other geophysical conditions, Proc. R. Soc. London A, 122, 456-486. HOOD, L.L., B.E. SOUKHAREV, M. FROMM and J.P. MCCORMACK (2001): Origin of extreme ozone minima at middle to high northern latitudes, J. Geophys. Res., 106 (D18), 20,925-20,940. JEANNET, P., R. STÜBI, G. LEVRAT, P. VIATTE and J. STAEHELIN (2007): Ozone balloon soundings at Payerne (Switzerland): reevaluation of the time series 1967-2002 and trend analysis, J. Geophys. Res., 112 (D11302), doi:10.1029/2005JD006862. KECKHUT, P., C. DAVID, M. MARCHAND, S. BEKKI, J. JUMELET and A. HAUCHECORNE (2007): Observation of Polar Stratospheric Clouds down to the Mediterranean coast, Atmos. Chem. Phys. Discuss., 7, 6557-6572. KEIL, M., D.R. JACKSON and M. C. HORT (2007): The January 2006 low ozone event over the U.K., Atmos. Chem. Phys., 7, 961-972. KOCH, G., H. WERNLI, J. STAEHELIN and T. PETER (2002): A lagrangian analysis of stratospheric ozone variability and long-term trends above Payerne (Switzerland) during 1970-2001, J. Geophys. Res., 107 (D19), 4373, doi:10.1029/2001jd001550. KOCH, G., H. WERNLI, C. SCHWIERZ, J. STAEHELIN and T. PETER (2005): A composite study on the structure and formation of ozone miniholes and minihighs over Central Europe, Geophys. Res. Lett., 32 (L12810), doi:10.1029/2004GL022062. MANNEY, G.L., W.H. DAFFER, K.B. STRAWBRIDGE, K.A. WALKER, C.D. BOONE, P.F. BERNATH, T. KERZENMACHER, M.J. SCHWARTZ, K. STRONG, R.J. SICA, K. KRÜGER, H.C. PUMPHREY, L. FROIDEVAUX, A. LAMBERT, M.L. SANTEE, N.J. LIVESEY, E.E. REMSBERG, M.G. MLYNCZAK and J.R. RUSSELL III (2007): The high Arctic in extreme winters: vortex, temperature, and MLS and ACE-FTS trace gas evolution, Atmos. Chem. Phys. Discuss., 7, 10235-10285. MUSCARI, G., A. G. DI SARRA, R. L. DE ZAFRA, F. LUCCI, F. BAORDO, F. ANGELINI and G. FIOCCO (2007): Middle atmospheric O3, CO, N2O, HNO3, and temperature profiles during the warm Arctic winter 2001-2002, J. Geophys. Res., 112 (D14304), doi:10.1029/2006JD007849. PARRISH, A., R.L. DE ZAFRA, P.M. SOLOMON and J.W. BARRETT (1988): A ground-based technique for millimeter wave spectroscopic observations of stratospheric trace constituents, Radio Sci., 23, 106-118. SCHOEBERL, M.R. and L.C. SPARLING (1995): Trajectory modelling, in ‘Diagnostic Tools in Atmospheric Physics’, Proceedings of the International School of Physics «Enrico Fermi», edited by G. FIOCCO and G. VISCONTI (Elsevier, New York), 124, 289-305. STICK, C., K. KRÜGER, N.H. SCHADE, H. SANDMANN and A. MACKE (2006): Episode of unusual high solar ultraviolet radiation over Central Europe due to dynamical reduced total ozone in May 2005, Atmos. Chem. Phys., 6, 1771-1776. TEITELBAUM, H., C. BASDEVANT, A. HERTZOG and N. SEMANE (2003): Comment on «A Lagrangian analysis of stratospheric ozone variability and long-term trends above Payerne (Switzerland) during 1970-2001» by G. KOCH, H. WERNLI, J. STAELIN and T. PETER, J. Geophys. Res., 108 (D21), 4674, doi:10.1029/2003JD003687. TWOMEY, S., B. HERMAN and R. RABINOFF (1977): An extension of the Chahine method of inverting the radiative transfer equation, J. Atmos. Sci., 34 (7), 1085-1090.
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spelling ftingv:oai:www.earth-prints.org:2122/3678 2023-05-15T14:28:14+02:00 Millimeter wave spectroscopic measurements of stratospheric and mesospheric constituents over the Italian Alps: stratospheric ozone Muscari, G. Cesaroni, C. Bianchi, C. de Zafra, R. L. Di Iorio, T. Fiorucci, I. Fuà, D. Romaniello, V. Zuccheretti, E. Muscari, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Cesaroni, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Bianchi, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia de Zafra, R. L.; Department of Physics and Astronomy and Institute for Terrestrial and Planetary Atmospheres, Di Iorio, T.; Dipartimento di Fisica, Università degli Studi di Roma «La Sapienza», Roma, Italy Fiorucci, I.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Fuà, D.; Dipartimento di Fisica, Università degli Studi di Roma «La Sapienza», Roma, Italy Romaniello, V.; Dipartimento di Fisica, Università degli Studi di Roma «La Sapienza», Roma, Italy Zuccheretti, E.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Department of Physics and Astronomy and Institute for Terrestrial and Planetary Atmospheres, Dipartimento di Fisica, Università degli Studi di Roma «La Sapienza», Roma, Italy 2007-06 http://hdl.handle.net/2122/3678 en eng Editrice Compositori Annals of Geophysics 3/50 (2007) BRAATHEN, G. (2006): Joint WMO/EU Arctic Ozone Bulletin, Winter/Spring Summary (World Meteorological Organization/European Ozone Research Coordinating Unit), Tech. Rep. 2006-1 (available on line at: <http://www.wmo.int/pages/prog/arep/gaw/ozone/in dex.html>). CHENG, D., R.L. DE ZAFRA and C. TRIMBLE (1996): Millimeter wave spectroscopic measurements over the South Pole, 2. An 11-month cycle of stratospheric ozone observations during 1993-1994, J. Geophys. Res., 101, 6781- 6793. DE ZAFRA, R.L. (1995): The ground-based measurements of stratospheric trace gases using quantitative millimeter wave emission spectroscopy, in ‘Diagnostic Tools in Atmospheric Physics’, Proceedings of the International School of Physics «Enrico Fermi», edited by G. FIOCCO and G. VISCONTI (Elsevier, New York), 124, 23-54. DE ZAFRA, R.L. and G. MUSCARI (2004): CO as an important high-altitude tracer of dynamics in the polar stratosphere and mesosphere, J. Geophys. Res., 109 (D06105), doi:10.1029/2003JD004099. DE ZAFRA, R. L.,V. CHAN, S. CREWELL, C. TRIMBLE and J.M. REEVES (1997): Millimeter wave spectroscopic measurements over the South Pole, 3. The behavior of stratospheric nitric acid through polar fall, winter, and spring, J. Geophys. Res., 102, 1399-1410. DOBSON, G.M.B., D.N. HARRISON and J. LAWRENCE (1929): Measurements of the amount of ozone in the earth’s atmosphere and its relation to other geophysical conditions, Proc. R. Soc. London A, 122, 456-486. HOOD, L.L., B.E. SOUKHAREV, M. FROMM and J.P. MCCORMACK (2001): Origin of extreme ozone minima at middle to high northern latitudes, J. Geophys. Res., 106 (D18), 20,925-20,940. JEANNET, P., R. STÜBI, G. LEVRAT, P. VIATTE and J. STAEHELIN (2007): Ozone balloon soundings at Payerne (Switzerland): reevaluation of the time series 1967-2002 and trend analysis, J. Geophys. Res., 112 (D11302), doi:10.1029/2005JD006862. KECKHUT, P., C. DAVID, M. MARCHAND, S. BEKKI, J. JUMELET and A. HAUCHECORNE (2007): Observation of Polar Stratospheric Clouds down to the Mediterranean coast, Atmos. Chem. Phys. Discuss., 7, 6557-6572. KEIL, M., D.R. JACKSON and M. C. HORT (2007): The January 2006 low ozone event over the U.K., Atmos. Chem. Phys., 7, 961-972. KOCH, G., H. WERNLI, J. STAEHELIN and T. PETER (2002): A lagrangian analysis of stratospheric ozone variability and long-term trends above Payerne (Switzerland) during 1970-2001, J. Geophys. Res., 107 (D19), 4373, doi:10.1029/2001jd001550. KOCH, G., H. WERNLI, C. SCHWIERZ, J. STAEHELIN and T. PETER (2005): A composite study on the structure and formation of ozone miniholes and minihighs over Central Europe, Geophys. Res. Lett., 32 (L12810), doi:10.1029/2004GL022062. MANNEY, G.L., W.H. DAFFER, K.B. STRAWBRIDGE, K.A. WALKER, C.D. BOONE, P.F. BERNATH, T. KERZENMACHER, M.J. SCHWARTZ, K. STRONG, R.J. SICA, K. KRÜGER, H.C. PUMPHREY, L. FROIDEVAUX, A. LAMBERT, M.L. SANTEE, N.J. LIVESEY, E.E. REMSBERG, M.G. MLYNCZAK and J.R. RUSSELL III (2007): The high Arctic in extreme winters: vortex, temperature, and MLS and ACE-FTS trace gas evolution, Atmos. Chem. Phys. Discuss., 7, 10235-10285. MUSCARI, G., A. G. DI SARRA, R. L. DE ZAFRA, F. LUCCI, F. BAORDO, F. ANGELINI and G. FIOCCO (2007): Middle atmospheric O3, CO, N2O, HNO3, and temperature profiles during the warm Arctic winter 2001-2002, J. Geophys. Res., 112 (D14304), doi:10.1029/2006JD007849. PARRISH, A., R.L. DE ZAFRA, P.M. SOLOMON and J.W. BARRETT (1988): A ground-based technique for millimeter wave spectroscopic observations of stratospheric trace constituents, Radio Sci., 23, 106-118. SCHOEBERL, M.R. and L.C. SPARLING (1995): Trajectory modelling, in ‘Diagnostic Tools in Atmospheric Physics’, Proceedings of the International School of Physics «Enrico Fermi», edited by G. FIOCCO and G. VISCONTI (Elsevier, New York), 124, 289-305. STICK, C., K. KRÜGER, N.H. SCHADE, H. SANDMANN and A. MACKE (2006): Episode of unusual high solar ultraviolet radiation over Central Europe due to dynamical reduced total ozone in May 2005, Atmos. Chem. Phys., 6, 1771-1776. TEITELBAUM, H., C. BASDEVANT, A. HERTZOG and N. SEMANE (2003): Comment on «A Lagrangian analysis of stratospheric ozone variability and long-term trends above Payerne (Switzerland) during 1970-2001» by G. KOCH, H. WERNLI, J. STAELIN and T. PETER, J. Geophys. Res., 108 (D21), 4674, doi:10.1029/2003JD003687. TWOMEY, S., B. HERMAN and R. RABINOFF (1977): An extension of the Chahine method of inverting the radiative transfer equation, J. Atmos. Sci., 34 (7), 1085-1090. http://hdl.handle.net/2122/3678 open millimeter-wave spectroscopy stratospheric ozone isentropic transport 01. Atmosphere::01.01. Atmosphere::01.01.99. General or miscellaneous article 2007 ftingv https://doi.org/10.1029/2003JD004099 2022-07-29T06:04:51Z Measurements of rotational lines emitted by middle atmospheric trace gases have been carried out from the Alpine station of Testa Grigia (45.9°N, 7.7°E, elev. 3500 m) by means of a Ground-Based Millimeter-wave Spectrometer (GBMS). Observations of species such as O3, HNO3, CO, N2O, HCN, and HDO took place during 4 winter periods, from February 2004 to March 2007, for a total of 116 days of measurements grouped in about 18 field campaigns. By studying the pressure-broadened shape of emission lines the vertical distribution of the observed constituents is retrieved within an altitude range of ∼17-75 km, constrained by the 600 MHz pass band and the 65 kHz spectral resolution of the back-end spectrometer. This work discusses the behavior of stratospheric O3 during the entire period of operation at Testa Grigia. Mid-latitude O3 columnar content as estimated using GBMS measurements can vary by large amounts over a period of very few days, with the largest variations observed in December 2005, February 2006, and March 2006, confirming that the northern winter of 2005-2006 was characterized by a particularly intense planetary wave activity. The largest rapid variation from maximum to minimum O3 column values over Testa Grigia took place in December 2006 and reached a relative value of 72% with respect to the average column content for that period. During most GBMS observation times much of the variability is concentrated in the column below 20 km, with tropospheric weather systems and advection of tropical tropospheric air into the lower stratosphere over Testa Grigia having a large impact on the observed variations in column contents. Nonetheless, a wide variability is also found in middle stratospheric GBMS O3 measurements, as expected for mid-latitude ozone. We find that O3 mixing ratios at ∼32 km are very well correlated with the solar illumination experienced by air masses over the previous ∼15 days, showing that already at 32 km altitude ozone photochemistry dominates over transport processes. The correlation of ... Article in Journal/Newspaper Arctic Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) Journal of Geophysical Research: Atmospheres 109 D6 n/a n/a