The Hotel Payload 2 campaign: Overview of NO, O and electron density measurements in the upper mesosphere and lower thermosphere

被引:8
作者
Enell, Carl-Fredrik [1 ]
Hedin, Jonas [2 ]
Stegman, Jacek [2 ]
Witt, Georg [2 ]
Friedrich, Martin [3 ]
Singer, Werner [4 ]
Baumgarten, Gerd [4 ]
Kaifler, Bernd [4 ]
Hoppe, Ulf-Peter [5 ]
Gustavsson, Bjoern [6 ]
Brandstrom, Urban [7 ]
Khaplanov, Mikhail [2 ]
Kero, Antti [1 ]
Ulich, Thomas [1 ]
Turunen, Esa [8 ]
机构
[1] Univ Oulu, Sodankyla Geophys Observ, FIN-99600 Sodankyla, Finland
[2] Stockholm Univ, Dept Meteorol, Stockholm, Sweden
[3] Graz Univ Technol, A-8010 Graz, Austria
[4] Univ Rostock, Leibniz Inst Atmospher Phys, Kuhlungsborn, Germany
[5] Norwegian Def Res Estab, N-2007 Kjeller, Norway
[6] Univ Southampton, Southampton SO9 5NH, Hants, England
[7] Swedish Inst Space Phys, S-98128 Kiruna, Sweden
[8] European Incoherent Scatter Sci Assoc, Kiruna, Sweden
基金
芬兰科学院;
关键词
Nitric oxide; Oxygen; Ionosphere; UMLT; NIGHTGLOW CONTINUUM; CHEMISTRY; GREEN; AIRGLOW; MIDDLE; EISCAT;
D O I
10.1016/j.jastp.2011.01.001
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The ALOMAR eARI Hotel Payload 2 (HotPay 2) rocket campaign took place at Andoya Rocket Range, Norway, in January 2008. The rocket was launched on January 31, 2008 at 19:14 UT, when auroral activity appeared after a long geomagnetically quiet period. In this paper we present an overview of the HotPay 2 measurements of upper mesospheric and lower thermospheric (UMLT) electron, atomic oxygen (O) and nitric oxide (NO) densities. [O] and [NO] were retrieved from a set of three photometers, Night-Time Emissions from the Mesosphere and Ionosphere (NEMI). Faraday rotation receivers on the rocket and the EISCAT UHF incoherent scatter radar provided simultaneous electron density profiles, whereas the ALOMAR Na lidar and meteor radar measured the temperature profile and wind. The aurora was also observed with ground-based imagers. The retrieved oxygen number density profile has a maximum at 89 km, some 10 km lower than expected from earlier measurements and modelled profiles based on climatological averages (such as the MSIS model), and the retrieved NO densities are also lower than the expected. Satellite measurements indicate that subsidence over the winter pole controlled the densities. Quantitative chemistry model results based on climatological average atmospheric density and temperature profiles were, therefore, not in good agreement with the measured profiles. The Hotel Payload 2 measurements thus confirm the importance of downward transport from the thermosphere into the winter polar vortex. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:2228 / 2236
页数:9
相关论文
共 43 条
[1]   The air glow reaction NO+O+(M)-> NO(2)(*)+(M) at low pressures [J].
Becker, K. H. ;
Groth, W. ;
Thran, D. .
CHEMICAL PHYSICS LETTERS, 1970, 6 (06) :583-586
[2]   MECHANISM OF AIR-AFTERGLOW NO+O-]NO2+HNU [J].
BECKER, KH ;
THRAN, D ;
GROTH, W .
CHEMICAL PHYSICS LETTERS, 1972, 15 (02) :215-&
[3]   Atmospheric Chemistry Experiment (ACE):: Mission overview -: art. no. L15S01 [J].
Bernath, PF ;
McElroy, CT ;
Abrams, MC ;
Boone, CD ;
Butler, M ;
Camy-Peyret, C ;
Carleer, M ;
Clerbaux, C ;
Coheur, PF ;
Colin, R ;
DeCola, P ;
Bernath, PF ;
McElroy, CT ;
Abrams, MC ;
Boone, CD ;
Butler, M ;
Camy-Peyret, C ;
Carleer, M ;
Clerbaux, C ;
Coheur, PF ;
Colin, R ;
DeCola, P ;
DeMazière, M ;
Drummond, JR ;
Dufour, D ;
Evans, WFJ ;
Fast, H ;
Fussen, D ;
Gilbert, K ;
Jennings, DE ;
Llewellyn, EJ ;
Lowe, RP ;
Mahieu, E ;
McConnell, JC ;
McHugh, M ;
McLeod, SD ;
Michaud, R ;
Midwinter, C ;
Nassar, R ;
Nichitiu, F ;
Nowlan, C ;
Rinsland, CP ;
Rochon, YJ ;
Rowlands, N ;
Semeniuk, K ;
Simon, P ;
Skelton, R ;
Sloan, JJ ;
Soucy, MA ;
Strong, K .
GEOPHYSICAL RESEARCH LETTERS, 2005, 32 (15)
[4]  
Brandstrom U., 2003, IRF Sci. Rep., 279
[5]   Case study of the mesospheric and lower thermospheric effects of solar X-ray flares:: coupled ion-neutral modelling and comparison with EISCAT and riometer measurements [J].
Enell, C. -F. ;
Verronen, P. T. ;
Beharrell, M. J. ;
Vierinen, J. P. ;
Kero, A. ;
Seppala, A. ;
Honary, F. ;
Ulich, T. ;
Turunen, E. .
ANNALES GEOPHYSICAE, 2008, 26 (08) :2311-2321
[6]   Meteoric smoke particle properties derived using dual-beam Arecibo UHF observations of D-region spectra during different seasons [J].
Fentzke, J. T. ;
Janches, D. ;
Strelnikova, I. ;
Rapp, M. .
JOURNAL OF ATMOSPHERIC AND SOLAR-TERRESTRIAL PHYSICS, 2009, 71 (17-18) :1982-1991
[7]   Bite-outs and other depletions of mesospheric electrons [J].
Friedrich, Martin ;
Rapp, Markus ;
Plane, John M. C. ;
Torkar, Klaus M. .
JOURNAL OF ATMOSPHERIC AND SOLAR-TERRESTRIAL PHYSICS, 2011, 73 (14-15) :2201-2211
[8]   NIGHTGLOW CONTINUUM [J].
GADSDEN, M ;
MAROVICH, E .
JOURNAL OF ATMOSPHERIC AND TERRESTRIAL PHYSICS, 1973, 35 (09) :1601-1614
[9]   ETON-1 - A DATABASE PERTINENT TO THE STUDY OF ENERGY-TRANSFER IN THE OXYGEN NIGHTGLOW [J].
GREER, RGH ;
MURTAGH, DP ;
MCDADE, IC ;
DICKINSON, PHG ;
THOMAS, L ;
JENKINS, DB ;
STEGMAN, J ;
LLEWELLYN, EJ ;
WITT, G ;
MACKINNON, DJ ;
WILLIAMS, ER .
PLANETARY AND SPACE SCIENCE, 1986, 34 (09) :771-788
[10]   Use of O2 airglow for calibrating direct atomic oxygen measurements from sounding rockets [J].
Hedin, J. ;
Gumbel, J. ;
Stegman, J. ;
Witt, G. .
ATMOSPHERIC MEASUREMENT TECHNIQUES, 2009, 2 (02) :801-812