Simulation of submillimetre atmospheric spectra for characterising potential ground-based remote sensing observations

被引:3
作者
Turner, Emma C. [1 ,4 ]
Withington, Stafford [1 ]
Newnham, David A. [2 ]
Wadhams, Peter [3 ]
Jones, Anna E. [2 ]
Clancy, Robin [3 ]
机构
[1] Univ Cambridge, Cavendish Lab, Madingley Rd, Cambridge CB3 0HE, England
[2] British Antarctic Survey, High Cross, Madingley Rd, Cambridge CB3 0ET, England
[3] Univ Cambridge, Dept Appl Math & Theoret Phys, Wilberforce Rd, Cambridge CB3 0WA, England
[4] Met Off, FitzRoy Rd, Exeter EX1 3PB, Devon, England
基金
英国自然环境研究理事会;
关键词
WATER-VAPOR CONTINUUM; FOURIER-TRANSFORM SPECTROMETER; POLAR TROPOSPHERIC OZONE; MICROWAVE LIMB SOUNDER; EARTHS ENERGY-BALANCE; MEASURE CLOUD ICE; STRATOSPHERIC OZONE; AURA SATELLITE; MAUNA-KEA; EOS MLS;
D O I
10.5194/amt-9-5461-2016
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The submillimetre is an understudied region of the Earth's atmospheric electromagnetic spectrum. Prior technological gaps and relatively high opacity due to the prevalence of rotational water vapour lines at these wavelengths have slowed progress from a ground-based remote sensing perspective; however, emerging superconducting detector technologies in the fields of astronomy offer the potential to address key atmospheric science challenges with new instrumental methods. A site study, with a focus on the polar regions, is performed to assess theoretical feasibility by simulating the downwelling (zenith angle = 0 degrees) clear-sky submillimetre spectrum from 30 mm (10 GHz) to 150 mu m (2000 GHz) at six locations under annual mean, summer, winter, daytime, night-time and low-humidity conditions. Vertical profiles of temperature, pressure and 28 atmospheric gases are constructed by combining radiosonde, meteorological reanalysis and atmospheric chemistry model data. The sensitivity of the simulated spectra to the choice of water vapour continuum model and spectroscopic line database is explored. For the atmospheric trace species hypobromous acid (HOBr), hydrogen bromide (HBr), perhydroxyl radical (HO2) and nitrous oxide (N2O) the emission lines producing the largest change in brightness temperature are identified. Signal strengths, centre frequencies, bandwidths, estimated minimum integration times and maximum receiver noise temperatures are determined for all cases. HOBr, HBr and HO2 produce brightness temperature peaks in the mK to mu K range, whereas the N2O peaks are in the K range. The optimal submillimetre remote sensing lines for the four species are shown to vary significantly between location and scenario, strengthening the case for future hyperspectral instruments that measure over a broad wavelength range. The techniques presented here provide a framework that can be applied to additional species of interest and taken forward to simulate retrievals and guide the design of future submillimetre instruments.
引用
收藏
页码:5461 / 5485
页数:25
相关论文
共 119 条
  • [1] Halogen activation via interactions with environmental ice and snow in the polar lower troposphere and other regions
    Abbatt, J. P. D.
    Thomas, J. L.
    Abrahamsson, K.
    Boxe, C.
    Granfors, A.
    Jones, A. E.
    King, M. D.
    Saiz-Lopez, A.
    Shepson, P. B.
    Sodeau, J.
    Toohey, D. W.
    Toubin, C.
    von Glasow, R.
    Wren, S. N.
    Yang, X.
    [J]. ATMOSPHERIC CHEMISTRY AND PHYSICS, 2012, 12 (14) : 6237 - 6271
  • [2] Anderson G.P., 1986, AIR FORCE GEOPHYS LA
  • [3] [Anonymous], 2014, Fifth assessment report (AR5). Synthesis Report
  • [4] The POLARBEAR CMB Polarization Experiment
    Arnold, K.
    Ade, P. A. R.
    Anthony, A. E.
    Aubin, F.
    Boettger, D.
    Borrill, J.
    Cantalupo, C.
    Dobbs, M. A.
    Errard, J.
    Flanigan, D.
    Ghribi, A.
    Halverson, N.
    Hazumi, M.
    Holzapfel, W. L.
    Howard, J.
    Hyland, P.
    Jaffe, A.
    Keating, B.
    Kisner, T.
    Kermish, Z.
    Lee, A. T.
    Linder, E.
    Lungu, M.
    Matsumura, T.
    Miller, N.
    Meng, X.
    Myers, M.
    Nishino, H.
    O'Brient, R.
    O'Dea, D.
    Reichardt, C.
    Schanning, I.
    Shimizu, A.
    Shimmin, C.
    Shimon, M.
    Spieler, H.
    Steinbach, B.
    Stompor, R.
    Suzuki, A.
    Tomaru, T.
    Tran, H. T.
    Tucker, C.
    Quealy, E.
    Richards, P. L.
    Zahn, O.
    [J]. MILLIMETER, SUBMILLIMETER, AND FAR-INFRARED DETECTORS AND INSTRUMENTATION FOR ASTRONOMY V, 2010, 7741
  • [5] Austermann J.E., 2012, SPIE Proceedings, V8452, DOI DOI 10.1117/12.927286
  • [6] Noise equivalent power of background limited thermal detectors at submillimeter wavelengths
    Benford, DJ
    Hunter, TR
    Phillips, TG
    [J]. INTERNATIONAL JOURNAL OF INFRARED AND MILLIMETER WAVES, 1998, 19 (07): : 931 - 938
  • [7] Buehler S., 1996, IMPACT CONTINUUM EMI, P1
  • [8] Buehler SA, 2007, Q J ROY METEOR SOC, V133, P109, DOI [10.1002/qj.143, 10.1002/qJ.143]
  • [9] Observing ice clouds in the submillimeter spectral range: the CloudIce mission proposal for ESA's Earth Explorer 8
    Buehler, S. A.
    Defer, E.
    Evans, F.
    Eliasson, S.
    Mendrok, J.
    Eriksson, P.
    Lee, C.
    Jimenez, C.
    Prigent, C.
    Crewell, S.
    Kasai, Y.
    Bennartz, R.
    Gasiewski, A. J.
    [J]. ATMOSPHERIC MEASUREMENT TECHNIQUES, 2012, 5 (07) : 1529 - 1549
  • [10] ARTS, the atmospheric radiative transfer simulator
    Buehler, SA
    Eriksson, P
    Kuhn, T
    von Engeln, A
    Verdesa, C
    [J]. JOURNAL OF QUANTITATIVE SPECTROSCOPY & RADIATIVE TRANSFER, 2005, 91 (01) : 65 - 93