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Abstrakty
The expected influence of variability in atmospheric aerosol profiles on retrievals of aerosol optical thickness (AOT) from NOAA AVHRR measurements is analysed. In particular, the bias in the AOT retrieval due to the assumption of a climatological aerosol profile in the retrieval algorithm is studied. The bias is defined as the difference between AOT retrieved with an algorithm using a climatological aerosol profile, and the actual AOT employed in the calculations of radiances at the top of the atmosphere (TOA). The TOA radiances are simulated by means of the MODTRAN code for different aerosol profiles. Atmospheric conditions and solar and satellite angles used in the bias simulations are typical of the Baltic region. In the simulations, the maximum absolute value of the bias amounts to nearly 40% in channel 2 and 14% in channel 1 of AVHRR.
Czasopismo
Rocznik
Tom
Strony
165--184
Opis fizyczny
bibliogr. 19 poz., tab., wykr.
Twórcy
autor
- Institute of Oceanology, Polish Academy of Sciences, Powstańców Warszawy 55, PL-81-712 Sopot, Poland, ania@iopan.gda.pl
Bibliografia
- [1].Adler-Golden S. M., Levine R.Y., Berk A., Bernstein L. S., Anderson G.P., Pukall B., 1999, Detection of cirrus clouds at 1.13 microns in AVIRIS scenes over land, [in:] Optical spectroscopic techniques and instrumentation for atmospheric and space research III, A.M. Larar (ed.), Proc. SPIE, 3756, 368 -373.
- [2].d'Almeida G.A., Koepke P., Shettle E.P., 1991, Atmospheric aerosols: global climatology and radiative characteristics, A. Deepak Publ., Hampton, VA, 561 pp.
- [3].Berk A., Anderson G.P., Acharya P.K., Chetwynd J.H., Bernstein L. S., Shettle E.P., MatthewM .W., Alder-Golden S.M., 1999a,MODTRAN4 users manual, Air Force Res. Lab., Hanscom, AFB, MA., 93 pp.
- [4].Berk A., Anderson G.P., Bernstein L.S., Acharya P.K., Dothe H., Matthew M. W., Adler-Golden S.M., Chetwynd J.H., Jr., Richtsmeier S.C., Pukall B., Allred C. L., Jeong L. S., Hoke M. L., 1999b, MODTRAN4 radiative transfer modeling for atmospheric correction, [in:] Optical spectroscopic techniques and instrumentation for atmospheric and space research III, A.M. Larar (ed.), Proc. SPIE, 3756, 348-353.
- [5].Carlund T., Hakansson B., Land P., 2005, Aerosol optical depth over the Baltic Sea derived from AERONET and SeaWiFS measurements, Int. J. Remote Sens., 26 (2), 233-245.
- [6].Costa M. J., Silva A.M., Levizzani V., 2004, Aerosol characterization and direct radiative forcing assessment over the ocean. Part I: Methodology and sensitivity analysis, J. Appl. Meteorol., 43 (2), 1799-1817.
- [7].Dubovik O., King M.D., 2000, A flexible inversion algorithm for retrieval of aerosol optical properties from Sun and sky radiance measurements, J. Geophys. Res., 105 (D16), 20673-20696.
- [8].Dubovik O., Smirnov A., Holben B. N., King M.D., Kaufman Y. J., Eck T. F., Slutsker I., 2000, Accuracy assessments of aerosol optical properties retrieved from AERONET Sun and sky radiance measurements, J. Geophys. Res., 105 (D8), 9791-9806.
- [9].Dziewulska-Łosiowa A., 1991, Ozone in the atmosphere, PWN, Warszawa, 396 pp., (in Polish).
- [10].Formenti P., Reiner T., Sprung D., Andreae M.O., Wendisch M., Wex H., Kindred D., Dewey K., Kent J., Tzortziou M., Vasaras A., Zerefos C., 2002, STAAARTE-MED 1998 summer airborne measurements over the Aegean Sea,1. Aerosol particles and trace gases, J. Geophys. Res., 107 (D21), 4450, doi: 10.1029/2001JD001337.
- [11].Green R. O., Pavri B., Williams O., Chovit C., 1998, Inflight validation AVIRIS calibration in 1996 and 1997, Summ. 7th JPL Airborne Earth Science Workshop, JPL Publ., 1 (97-21), 193-203.
- [12].Kostyrko K., Szumowski J., Szerszeń A., 1986, Psychrometric and hygrometric tables, IMiGW, PWN, Warszaw a, 614 pp., (in Polish).
- [13].Kuśmierczyk-Michulec J., Rozwadowska A., 1999, Seasonal changes of the aerosol optical thickness for the atmosphere over the Baltic Sea - preliminary results, Oceanologia, 41 (2), 127-145.
- [14].Meloni D., di Sarra A., di Iorio T., Fiocco G., 2004, Direct radiative forcing of Saharan dust in the Mediterranean from measurements at Lampedusa Island and MISR space-borne observations, J. Geophys. Res., 109, D08206, doi: 10.1029/2003JD003960.
- [15].Meloni D., di Sarra A., di Iorio T., Fiocco G., 2005, Influence of the vertical profile of Saharan dust on the visible direct radiative forcing, J. Quant. Spectrosc. RA, 93 (4), 397-413.
- [16].Miętus M., 1998, The climate of the Baltic Sea Basin, Marine Meteorology and Related Oceanographic Activities, Rep. No 41, WMO/TD-No 933, 180 pp.
- [17].Mitchell R.M., O'Brien D.M., Campbell S.K., 2006, Characteristics and radiative impact of the aerosol generated by the Canberra firestorm of January 2003, J. Geophys. Res., 111, D02204, doi: 10.1029/2005JD006304.
- [18].Reitan G.H., 1960, Mean monthly values of precipitable water over the United States, Mon. Weather Rev., 88 (1), 25-35.
- [19].Woźniak S.B., 1996, Mathematical spectral model of solar irradiance reflectance and transmittance by a wind-ruffled sea surface. Part 1. The physical problem and mathematical apparatus, Oceanologia, 38 (4), 447-467.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS5-0003-0062