A new method for nocturnal aerosol measurements with a lunar photometer prototype

被引:63
作者
Barreto, A. [1 ]
Cuevas, E. [1 ]
Damiri, B. [2 ]
Guirado, C. [1 ,3 ,4 ]
Berkoff, T. [5 ]
Berjon, A. J. [1 ]
Hernandez, Y. [1 ]
Almansa, F. [1 ]
Gil, M. [6 ]
机构
[1] Meteorol State Agcy Spain AEMET, Izana Atmospher Res Ctr, Izana, Spain
[2] Cimel Elect, Paris, France
[3] Syst Spanish Natl Res Council CSIC, Inst Environm Assessment & Water Res, Barcelona, Spain
[4] Valladolid Univ GOA UVA, Atmospher Opt Grp, Valladolid, Spain
[5] Univ Maryland Baltimore Cty, Baltimore, MD 21228 USA
[6] INTA, Instrumentat & Atmospher Res Dept, Madrid, Spain
关键词
OPTICAL DEPTH; AERONET; CALIBRATION; IRRADIANCE; NETWORK; AFRICA; CLOUD;
D O I
10.5194/amt-6-585-2013
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
This paper presents the preliminary results of nocturnal Aerosol Optical Depth (tau(a)) and Angstrom Exponent (alpha) obtained from a new lunar photometer prototype, trade name Cimel CE-318U. Due to the variation of the moon's illumination inherent to the lunar cycle, the typical Langley-plot Method used in solar photometry to calibrate these instruments cannot be applied. In this paper, we propose three different methods to carry out the lunar-photometer calibration. In order to validate the results, we have selected three events which encompass seven nights and ten days under different atmospheric conditions, including several saharan dust intrusions episodes. Method#1 is introduced in this work as a modification of the usual Langley Method. This technique, called Lunar-Langley Method, requires the extraterrestrial irradiances from a lunar irradiance model, providing similar accuracies on tau(a) to those of AERONET (+/- 0.01-0.02). It makes comparable daytime and nighttime measurements. Method#2 consists of transferring the current calibration from a master used by sunphotometers. Its results are again within the limit of accuracy expected for the instrument. Method#3 uses an integrating sphere and the methodology proposed by Li et al. (2008) to determine sky calibration coefficients (C-j) and the instrument's solid angle field-of-view (Omega), respectively. We observe significant tau(a) differences between Method#1 and #3 (up to 0.07), which might be attributed to the errors propagation in Method#3. The good results obtained from the comparison against a second CE-318U prototype, and against daytime data from a Precision Filter Radiometer (PFR), constitute a valuable assessment of CE-318U performance. Results of alpha and its spectral variation (delta alpha) show good agreement between daytime and nighttime, being able to identify the aerosol properties associated with each event.
引用
收藏
页码:585 / 598
页数:14
相关论文
共 27 条
[1]  
Angstrom A., 1929, GEOGR ANN, V11, P156, DOI [DOI 10.2307/519399, 10.2307/519399]
[2]   Aerosol characterization in Northern Africa, Northeastern Atlantic, Mediterranean Basin and Middle East from direct-sun AERONET observations [J].
Basart, S. ;
Perez, C. ;
Cuevas, E. ;
Baldasano, J. M. ;
Gobbi, G. P. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2009, 9 (21) :8265-8282
[3]   Nocturnal Aerosol Optical Depth Measurements with a Small-Aperture Automated Photometer Using the Moon as a Light Source [J].
Berkoff, Timothy A. ;
Sorokin, Mikail ;
Stone, Tom ;
Eck, Thomas F. ;
Hoff, Raymond ;
Welton, Ellsworth ;
Holben, Brent .
JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY, 2011, 28 (10) :1297-1306
[4]  
Campbell JR, 2002, J ATMOS OCEAN TECH, V19, P431, DOI 10.1175/1520-0426(2002)019<0431:FTESCA>2.0.CO
[5]  
2
[6]   Wavelength dependence of the optical depth of biomass burning, urban, and desert dust aerosols [J].
Eck, TF ;
Holben, BN ;
Reid, JS ;
Dubovik, O ;
Smirnov, A ;
O'Neill, NT ;
Slutsker, I ;
Kinne, S .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1999, 104 (D24) :31333-31349
[7]   Optical calibration facility at the Izana Atmospheric Research Center [J].
Guirado, C. ;
Ramos, R. ;
de Frutos, A. ;
Berjon, A. ;
Redondas, A. ;
Lopez, C. ;
Cachorro, V. ;
Cuevas, E. ;
Gonzalez, R. ;
Gonzalez, S. ;
Hernandez, M. .
OPTICA PURA Y APLICADA, 2012, 45 (01) :57-62
[8]   Continuous day and night aerosol optical depth observations in the Arctic between 1991 and 1999 [J].
Herber, A ;
Thomason, LW ;
Gernandt, H ;
Leiterer, U ;
Nagel, D ;
Schulz, KH ;
Kaptur, J ;
Albrecht, T ;
Notholt, J .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2002, 107 (D10)
[9]   AERONET - A federated instrument network and data archive for aerosol characterization [J].
Holben, BN ;
Eck, TF ;
Slutsker, I ;
Tanre, D ;
Buis, JP ;
Setzer, A ;
Vermote, E ;
Reagan, JA ;
Kaufman, YJ ;
Nakajima, T ;
Lavenu, F ;
Jankowiak, I ;
Smirnov, A .
REMOTE SENSING OF ENVIRONMENT, 1998, 66 (01) :1-16
[10]   SIZE DISTRIBUTION AND SCATTERING PHASE FUNCTION OF AEROSOL-PARTICLES RETRIEVED FROM SKY BRIGHTNESS MEASUREMENTS [J].
KAUFMAN, YJ ;
GITELSON, A ;
KARNIELI, A ;
GANOR, E ;
FRASER, RS ;
NAKAJIMA, T ;
MATTOO, S ;
HOLBEN, BN .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1994, 99 (D5) :10341-10356