Status of aqua MODIS on-orbit calibration and characterization

被引:15
作者
Xiong, X [1 ]
Barnes, W [1 ]
Chiang, K [1 ]
Erives, H [1 ]
Che, N [1 ]
Sun, J [1 ]
Isaacman, A [1 ]
Salomonson, V [1 ]
机构
[1] NASA, Goddard Space Flight Ctr, Earth Sci Directorate, Greenbelt, MD 20771 USA
来源
SENSORS, SYSTEMS, AND NEXT-GENERATION SATELLITES VIII | 2004年 / 5570卷
关键词
aqua; Terra; MODIS; solar diffuser; SRCA; blackbody; calibration; radiometty; uncertainty;
D O I
10.1117/12.564940
中图分类号
V [航空、航天];
学科分类号
08 ; 0825 ;
摘要
The MODIS Flight Model 1 (FM1) has been in operation for more than two years since its launch onboard the NASA's Earth Observing System (EOS) Aqua spacecraft on May 4, 2002. The MODIS has 36 spectral bands: 20 reflective solar bands (RSB) with center wavelengths from 0.41 to 2.2mum and 16 thermal emissive bands (TEB) from 3.7 to 14.5mum. It provides the science community observations (data products) of the Earth's land, oceans, and atmosphere for a board range of applications. Its primary on-orbit calibration and characterization activities are performed using a solar diffuser (SD) and a solar diffuser stability monitor (SDSM) system for the RSB and a blackbody for the TEB. Another on-board calibrator (OBC) known as the spectro-radiometric calibration assembly (SRCA) is used for the instrument's spatial (TEB and RSB) and spectral (RSB only) characterization. We present in this paper the status of Aqua MODIS calibration and characterization during its first two years of on-orbit operation. Discussions will be focused on the calibration activities executed on-orbit in order to maintain and enhance the instrument's performance and the quality of its Level 113 (LIB) data products. We also provide comparisons between Aqua MODIS and Terra MODIS (launched in December, 1999), including their similarity and difference in response trending and optics degradation. Existing data and results show that Aqua MODIS bands 8 (0.412mum) and 9 (0.443mum) have much smaller degradation than Terra MODIS bands 8 and 9. The most noticeable feature shown in the RSB trending is that the mirror side differences in Aqua MODIS are extremely small and stable (<0.1%) while the Terra MODIS RSB trending has shown significant mirror side difference and wavelength dependent degradation. The overall stability of the Aqua MODIS TEB is also better than that of the Terra MODIS during their first two years of on-orbit operation.
引用
收藏
页码:317 / 327
页数:11
相关论文
共 19 条
[1]  
Barnes W. L., 1993, Crit. Rev. Opt. Sci. Technol, VCR47, P285, DOI DOI 10.1117/12.161578
[2]   Status of Terra MODIS and Aqua MODIS [J].
Barnes, WL ;
Xiong, X ;
Salomonson, VV .
CALIBRATION, CHARACTERIZATION OF SATELLITE SENSORS, PHYSICAL PARAMETERS DERIVED FROM SATELLITE DATA, 2003, 32 (11) :2099-2106
[3]  
BARNES WL, 2002, P IGARSS
[4]  
BARNES WL, 2003, P SPIE EARTH OBSERVI, V8, P5151
[5]   An overview of MODIS capabilities for ocean science observations [J].
Esaias, WE ;
Abbott, MR ;
Barton, I ;
Brown, OB ;
Campbell, JW ;
Carder, KL ;
Clark, DK ;
Evans, RH ;
Hoge, FE ;
Gordon, HR ;
Balch, WM ;
Letelier, R ;
Minnett, PJ .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 1998, 36 (04) :1250-1265
[6]   The Moderate Resolution Imaging Spectroradiometer (MODIS): Land remote sensing for global change research [J].
Justice, CO ;
Vermote, E ;
Townshend, JRG ;
Defries, R ;
Roy, DP ;
Hall, DK ;
Salomonson, VV ;
Privette, JL ;
Riggs, G ;
Strahler, A ;
Lucht, W ;
Myneni, RB ;
Knyazikhin, Y ;
Running, SW ;
Nemani, RR ;
Wan, ZM ;
Huete, AR ;
van Leeuwen, W ;
Wolfe, RE ;
Giglio, L ;
Muller, JP ;
Lewis, P ;
Barnsley, MJ .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 1998, 36 (04) :1228-1249
[7]   Cloud and aerosol properties, precipitable water, and profiles of temperature and water vapor from MODIS [J].
King, MD ;
Menzel, WP ;
Kaufman, YJ ;
Tanré, D ;
Gao, BC ;
Platnick, S ;
Ackerman, SA ;
Remer, LA ;
Pincus, R ;
Hubanks, PA .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 2003, 41 (02) :442-458
[8]   Determination of the spatial characteristics by using the Spectro-Radiometric Calibration Assembly (SRCA) of MODIS (Part 1. Along-scan) [J].
Montgomery, H ;
Che, NZ ;
Bowser, J .
EARTH OBSERVING SYSTEMS III, 1998, 3439 :226-237
[9]   Determination of the spatial characteristics by using the Spectro-Radiometric Calibration Assembly (SRCA) of MODIS (Part II. Along-track) [J].
Montgomery, H ;
Che, NZ ;
Bowser, J .
EARTH OBSERVING SYSTEMS III, 1998, 3439 :238-246
[10]  
MONTGOMERY H, 2002, IEEE GEOSCI REMOTE S, V38, P877