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9 | <CENTER><P><B><FONT COLOR="#0000FF"><FONT SIZE=+2>GEISA aerosol databank</FONT></FONT></B></P></CENTER> |
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10 | |
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11 | <P>The next edition of the GEISA spectroscopic databanks will contain aerosol |
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12 | data files: </P> |
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13 | |
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14 | <CENTER><P><B><FONT SIZE=+2>I.</FONT></B> </P></CENTER> |
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15 | |
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16 | <P><FONT COLOR="#FF0000">Integral optical characteristics (e.g. <I>extinction |
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17 | coefficient, scattering phase function, etc..</I>.) of the basic aerosol |
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18 | components (e.g. <I>Dust-Like, Water-Soluble, Soot, Volcanic ash, etc...</I>) |
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19 | as well as files with refractive indices of some aerosol constituents: |
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20 | </FONT></P> |
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21 | |
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22 | <P>Rublev A.N., Algoritms and the calculation of the aerosol phase functions. |
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23 | Preprint IAE-5715/16, Russian Research Center "Kurchatov Institut", |
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24 | Moscow, 1994. (in Russian).</P> |
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25 | |
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26 | <P>A preliminary cloudless standard atmosphere for radiation computation. |
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27 | World Climate Research Program , WCP-112, WMO/TD-NO. 24, World Meteorological |
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28 | Organization, March 1986. </P> |
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29 | |
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30 | <CENTER><P><B><FONT SIZE=+2>II.</FONT></B></P></CENTER> |
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31 | |
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32 | <P><FONT COLOR="#FF0000">Aerosol data in HITRAN standard format (same content |
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33 | as HITRAN-96):</FONT></P> |
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34 | |
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35 | <P><B>Real and imaginary indices of refraction for water at 27 C between |
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36 | 10 and 5000 cm<SUP>-1</SUP> :</B></P> |
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37 | |
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38 | <P>Downing H.D., and Williams D., Optical constants of water in the infrared, |
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39 | <I>J.Geophys.Res. </I>, 1975, <B>80</B>, 1656-1661. </P> |
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40 | |
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41 | <P><B>Imaginary indices of refraction for water and ice in the 0.67 to |
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42 | 2.5 micron range:</B></P> |
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43 | |
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44 | <P>Kou L., Labrie D., and Chylek P., Refractive indices of water and ice |
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45 | in the 0.65 to 2.5 micron range, <I>Appl.Opt.</I> 1993, <B>32</B>, 3531-3540. |
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46 | </P> |
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47 | |
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48 | <P><B>Real and imaginary indices of refraction of ice at -7 C for the 4.43e-2 |
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49 | to 167 micron range, and indices of ice at -1, -5, -20, and -60 C for the |
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50 | 167 to 8.6e6 micron range:</B></P> |
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51 | |
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52 | <P>Warren S.G., Optical constants of ice from the ultraviolet to the microwave, |
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53 | <I>Appl.Opt.</I>, 1994, <B>23</B>, 1206-1225. </P> |
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54 | |
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55 | <P><B>Real and imaginary indices of refraction for water, ice, sodium chloride, |
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56 | sea salt, water soluble aerosol, ammonium sulfate, carbonaceous aerosol, |
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57 | volcanic dust, sulfuric acid, meteoric dust, quartz, hematite, sand, and |
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58 | dust-like aerosol.</B> </P> |
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59 | |
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60 | <P>The data were tabulated by E.P. Shettle of the Naval Research Laboratory. |
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61 | </P> |
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62 | |
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63 | <P><B>Real and imaginary indices of refraction of nitric acid trihydrate, |
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64 | nitric acid dihydrate, nitric acid monohydrate, and solid amorphous nitric |
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65 | acid solutions:</B></P> |
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66 | |
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67 | <P>Toon O.B., Tolbert M.A., Koehler B.C., Middlebrook A.M., and Jordan |
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68 | J., The infrared optical constants of H<SUB>2</SUB>O-icd, amorphous nitric |
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69 | acid solutions, and nitric acid hydrates, <I>J.Geophys.Res</I>. (in press, |
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70 | 1994). </P> |
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71 | |
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72 | <P><B>Real and imaginary indices of refraction of sulfuric acid solutions |
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73 | at 25, 38, 50, 75, 84.5, and 95.6% H<SUB>2</SUB>SO<SUB>4</SUB>, by weight:</B></P> |
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74 | |
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75 | <P>Palmer K.F. and Dudley Williams, Optical constants of sulfuric acid; |
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76 | Application to the clouds of Venus?, <I>Appl.Opt.</I>, 1975, <B>14</B>, |
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77 | 208-219. </P> |
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78 | |
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79 | <P><B>Real and imaginary indices of refraction of sulfuric acid solutions |
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80 | at 75 and 90% H<SUB>2</SUB>SO<SUB>4</SUB>, by weight, plus the standard |
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81 | deviations of the measurements. Real and imaginary indices of refraction |
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82 | of nitric acid solutions at 68% HNO<SUB>3</SUB>, by weight, plus the standard |
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83 | deviations of the measurements:</B></P> |
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84 | |
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85 | <P>Remsberg E.E., Lavery D., and Crawford B., Optical constants for sulfuric |
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86 | and nitric acids, <I>J.Chem. and Engin.Data </I>, 1974, <B>19</B>, 263-255. |
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87 | </P> |
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88 | |
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89 | <P><B>Theoretical equilibrium composition (weight percentage of H<SUB>2</SUB>SO<SUB>4</SUB>) |
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90 | of sulfuric acid solutions, given as a function of temperature and H<SUB>2</SUB>O |
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91 | vapour pressure:</B> </P> |
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92 | |
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93 | <P>Steele H.M., and Hamill P., Effects of temperature and humidity on the |
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94 | growth and optical properties of sulphuric acid-water droplets in the stratosphere, |
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95 | <I>J.Aerosol Sci</I>., 1981, <B>12</B>, 517-528.</P> |
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96 | |
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97 | <P><B>Sulfuric acid density (gm/cm<SUP>3</SUP>) values for solutions between |
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98 | 0 and 100% H<SUB>2</SUB>SO<SUB>4</SUB> (by weight) for temperatures between |
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99 | 0 and 60 C:</B></P> |
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100 | |
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101 | <P>Timmermans J., The physico-chemical constants of binary systems in concentrated |
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102 | solutions, Interscience, New York, (1960). </P> |
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103 | |
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104 | <P><B>Real and imaginary indices of refraction of H<SUB>2</SUB>O-ice, amorphous |
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105 | nitric acid solutions, and nitric acid hydrates: </B></P> |
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106 | |
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107 | <P>Toon O.B., Tolbert M.A., Koehler B.C., Middlebrook A.M., and Jordan |
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108 | J., The infrared optical constants of H<SUB>2</SUB>O-ice, amorphous acid |
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109 | solutions, and nitric acid hydrates, <I>J.Geophys.Res.</I> (in press 1994). |
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110 | </P> |
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111 | |
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