Use of CRISTA mesopause region temperatures for the intercalibration of ground-based instruments
Most available ground-based (GB) techniques for measuring temperatures in the upper mesosphere to lower thermosphere (or mesopause region) have systematic errors that are comparable to those of orbiting instruments. Determining these unknown biasses would normally require colocated observations that...
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2006
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| LEADER | 12685caa a22011057a 4500 | ||
|---|---|---|---|
| 001 | PAPER-21752 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205314.0 | ||
| 008 | 190411s2006 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-33748965602 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Scheer, J. | |
| 245 | 1 | 0 | |a Use of CRISTA mesopause region temperatures for the intercalibration of ground-based instruments |
| 260 | |c 2006 | ||
| 270 | 1 | 0 | |m Scheer, J.; Instituto de Astronomía y Física del Espacio, CONICET-UBA, Buenos Aires, Argentina; email: jurgen@caerce.edu.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 504 | |a Oberheide, J., Hagan, M., Ward, W.E., Riese, M., Offermann, D., Modeling the diurnal tide for the Cryogenic Infrared Spectrometers and Telescopes for the Atmosphere (CRISTA) 1 time period (2000) Journal of Geophysical Research, 105 (A11), pp. 24,917-24,929 | ||
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| 504 | |a Reisin, E.R., Scheer, J., Searching for trends in mesopause region airglow intensities and temperatures at El Leoncito (2002) Physics and Chemistry of the Earth, 27 (6-8), pp. 563-569 | ||
| 504 | |a Reisin, E.R., Scheer, J., Gravity wave activity in the mesopause region from airglow measurements at El Leoncito (2004) Journal of Atmospheric and Solar-Terrestrial Physics, 66 (6-9), pp. 655-661 | ||
| 504 | |a Riese, M., Spang, R., Preusse, P., Ern, M., Jarisch, M., Offermann, D., Grossmann, K.-U., Cryogenic Infrared Spectrometers and Telescopes for the Atmosphere (CRISTA) data processing and atmospheric temperature and trace gas retrieval (1999) Journal of Geophysical Research, 104, pp. 16,349-16,367 | ||
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| 504 | |a von Savigny, C., Eichmann, K.-U., Llewellyn, E.J., Bovensmann, H., Burrows, J.P., Bittner, M., Höppner, K., Winkler, P., First near-global retrievals of OH rotational temperatures from satellite-based Meinel band emission measurements (2004) Geophysical Research Letters, 31, pp. L15111. , 10.1029/2004GL020410 | ||
| 504 | |a Ward, W.E., Oberheide, J., Riese, M., Preusse, P., Offermann, D., Tidal signatures in temperature data from CRISTA 1 mission (1999) Journal of Geophysical Research, 104, pp. 16,391-16,403 | ||
| 504 | |a Ward, W.E., Oberheide, J., Riese, M., Preusse, P., Offermann, D., Planetary wave two signatures in CRISTA 2 ozone and temperature data (2000) Geophysical Monographs, 123, pp. 319-325 | ||
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| 520 | 3 | |a Most available ground-based (GB) techniques for measuring temperatures in the upper mesosphere to lower thermosphere (or mesopause region) have systematic errors that are comparable to those of orbiting instruments. Determining these unknown biasses would normally require colocated observations that are only seldom feasible. Satellite measurements can be used as a "transfer standard" between GB observations that are not colocated. In this context, even with a reproducible or known bias in the satellite data, the comparison is still meaningful. Since Cryogenic Infrared Spectrometers and Telescopes for the Atmosphere (CRISTA) temperatures cover the mesopause region with very good accuracy (statistical errors do not exceed 1.5 K and systematic uncertainties range from about 3-7.5 K), they are quite suitable for this purpose. Because of the nearly constant precision over the height range of interest, also rotational temperatures of airglow emissions from different altitudes like the OH and O2 bands (or the OI 558 nm line) can be successfully compared with each other. In spite of the limited number of overpasses during the relatively short CRISTA missions, the feasibility of such an intercalibration is demonstrated for widely separated GB sites. Here, the results obtained for GB measurements at eight different sites, using CRISTA-1 and CRISTA-2 data, are presented. For OH temperatures, the standard deviation between the different instruments is only 5.4 K, confirming previous estimates. © 2006 Elsevier Ltd. All rights reserved. |l eng | |
| 536 | |a Detalles de la financiación: Bundesministerium für Bildung und Forschung | ||
| 536 | |a Detalles de la financiación: Deutsches Zentrum für Luft- und Raumfahrt, NSF-ATM-0109353 | ||
| 536 | |a Detalles de la financiación: Agencia Nacional de Promoción Científica y Tecnológica, PICT 12187 | ||
| 536 | |a Detalles de la financiación: The authors wish to acknowledge the active participation of the many ground-based observers taking part in the two campaigns that accompanied the two CRISTA/MAHRSI missions, as well as those colleagues who supplied data that could not be included here for not meeting the overpass conditions. Valuable help by M. Jarisch about the use of the CRISTA data base program GLOBAL is gratefully acknowledged. The CRISTA project is funded by grant 50 QV 9802-4 of the Bundesministerium für Bildung und Forschung (BMBF, Bonn, Germany) through Deutsches Zentrum für Luft- und Raumfahrt (DLR, Bonn). The first author thanks his hosts for the opportunity to work during 1 month as invited scientist at the University of Wuppertal. The observations from Mount John Observatory were supported by grant NSF-ATM-0109353. J.S. and E.R.R. acknowledge funding through ANPCyT grant PICT 12187. | ||
| 593 | |a Instituto de Astronomía y Física del Espacio, CONICET-UBA, Buenos Aires, Argentina | ||
| 593 | |a Physics Department, University of Wuppertal, Wuppertal, Germany | ||
| 593 | |a Space and Atmospheric Sciences, Australian Antarctic Division, Kingston, TAS, Australia | ||
| 593 | |a Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195-1310, United States | ||
| 593 | |a Electrical and Computer Engineering, Utah State University, 6 Fairlane Terrace, Winchester, MA 01890, United States | ||
| 593 | |a Institute of Cosmophysical Research and Aeronomy, Yakutsk, Russian Federation | ||
| 690 | 1 | 0 | |a AIRGLOW |
| 690 | 1 | 0 | |a MESOPAUSE REGION |
| 690 | 1 | 0 | |a SATELLITE |
| 690 | 1 | 0 | |a TEMPERATURE |
| 690 | 1 | 0 | |a CALIBRATION |
| 690 | 1 | 0 | |a EARTH ATMOSPHERE |
| 690 | 1 | 0 | |a INFRARED SPECTROMETERS |
| 690 | 1 | 0 | |a PHOTOCHEMICAL REACTIONS |
| 690 | 1 | 0 | |a PROBABILITY DENSITY FUNCTION |
| 690 | 1 | 0 | |a SATELLITE GROUND STATIONS |
| 690 | 1 | 0 | |a THERMODYNAMIC STABILITY |
| 690 | 1 | 0 | |a WEATHER SATELLITES |
| 690 | 1 | 0 | |a AIRGLOW EMISSION |
| 690 | 1 | 0 | |a MESOPAUSE REGION |
| 690 | 1 | 0 | |a STANDARD DEVIATION |
| 690 | 1 | 0 | |a ATMOSPHERIC TEMPERATURE |
| 690 | 1 | 0 | |a AIR TEMPERATURE |
| 690 | 1 | 0 | |a CALIBRATION |
| 690 | 1 | 0 | |a GROUND-BASED MEASUREMENT |
| 690 | 1 | 0 | |a MESOPAUSE |
| 690 | 1 | 0 | |a SATELLITE DATA |
| 700 | 1 | |a Reisin, E.R. | |
| 700 | 1 | |a Gusev, O.A. | |
| 700 | 1 | |a French, W.J.R. | |
| 700 | 1 | |a Hernandez, G. | |
| 700 | 1 | |a Huppi, R. | |
| 700 | 1 | |a Ammosov, P. | |
| 700 | 1 | |a Gavrilyeva, G.A. | |
| 700 | 1 | |a Offermann, D. | |
| 773 | 0 | |d 2006 |g v. 68 |h pp. 1698-1708 |k n. 15 |p J. Atmos. Sol.-Terr. Phys. |x 13646826 |w (AR-BaUEN)CENRE-5432 |t Journal of Atmospheric and Solar-Terrestrial Physics | |
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| 856 | 4 | 0 | |u https://hdl.handle.net/20.500.12110/paper_13646826_v68_n15_p1698_Scheer |y Handle |
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| 963 | |a VARI | ||