source: ether_geisa/trunk/htdocs/geisa_aerosupd_gs03.html @ 356

Last change on this file since 356 was 1, checked in by cbipsl, 18 years ago

Geisa inital import
File size: 5.3 KB
Line 
1<!DOCTYPE HTML PUBLIC "-//W3C//DTD HTML 3.2//EN">
2<HTML>
3<HEAD>
4   <TITLE></TITLE>
5   <META NAME="GENERATOR" CONTENT="Mozilla/3.01Gold (X11; I; SunOS 4.1.4 sun4m) [Netscape]">
6</HEAD>
7<BODY>
8
9<CENTER><P><B><FONT COLOR="#0000FF"><FONT SIZE=+2>GEISA aerosol databank</FONT></FONT></B></P></CENTER>
10
11<P>The next edition of the GEISA spectroscopic databanks will contain aerosol
12data files: </P>
13
14<CENTER><P><B><FONT SIZE=+2>I.</FONT></B> </P></CENTER>
15
16<P><FONT COLOR="#FF0000">Integral optical characteristics (e.g. <I>extinction
17coefficient, scattering phase function, etc..</I>.) of the basic aerosol
18components (e.g. <I>Dust-Like, Water-Soluble, Soot, Volcanic ash, etc...</I>)
19as well as files with refractive indices of some aerosol constituents:
20</FONT></P>
21
22<P>Rublev A.N., Algoritms and the calculation of the aerosol phase functions.
23Preprint IAE-5715/16, Russian Research Center &quot;Kurchatov Institut&quot;,
24Moscow, 1994. (in Russian).</P>
25
26<P>A preliminary cloudless standard atmosphere for radiation computation.
27World Climate Research Program , WCP-112, WMO/TD-NO. 24, World Meteorological
28Organization, March 1986. </P>
29
30<CENTER><P><B><FONT SIZE=+2>II.</FONT></B></P></CENTER>
31
32<P><FONT COLOR="#FF0000">Aerosol data in HITRAN standard format (same content
33as HITRAN-96):</FONT></P>
34
35<P><B>Real and imaginary indices of refraction for water at 27 C between
3610 and 5000 cm<SUP>-1</SUP> :</B></P>
37
38<P>Downing H.D., and Williams D., Optical constants of water in the infrared,
39<I>J.Geophys.Res. </I>, 1975, <B>80</B>, 1656-1661. </P>
40
41<P><B>Imaginary indices of refraction for water and ice in the 0.67 to
422.5 micron range:</B></P>
43
44<P>Kou L., Labrie D., and Chylek P., Refractive indices of water and ice
45in the 0.65 to 2.5 micron range, <I>Appl.Opt.</I> 1993, <B>32</B>, 3531-3540.
46</P>
47
48<P><B>Real and imaginary indices of refraction of ice at -7 C for the 4.43e-2
49to 167 micron range, and indices of ice at -1, -5, -20, and -60 C for the
50167 to 8.6e6 micron range:</B></P>
51
52<P>Warren S.G., Optical constants of ice from the ultraviolet to the microwave,
53<I>Appl.Opt.</I>, 1994, <B>23</B>, 1206-1225. </P>
54
55<P><B>Real and imaginary indices of refraction for water, ice, sodium chloride,
56sea salt, water soluble aerosol, ammonium sulfate, carbonaceous aerosol,
57volcanic dust, sulfuric acid, meteoric dust, quartz, hematite, sand, and
58dust-like aerosol.</B> </P>
59
60<P>The data were tabulated by E.P. Shettle of the Naval Research Laboratory.
61</P>
62
63<P><B>Real and imaginary indices of refraction of nitric acid trihydrate,
64nitric acid dihydrate, nitric acid monohydrate, and solid amorphous nitric
65acid solutions:</B></P>
66
67<P>Toon O.B., Tolbert M.A., Koehler B.C., Middlebrook A.M., and Jordan
68J., The infrared optical constants of H<SUB>2</SUB>O-icd, amorphous nitric
69acid solutions, and nitric acid hydrates, <I>J.Geophys.Res</I>. (in press,
701994). </P>
71
72<P><B>Real and imaginary indices of refraction of sulfuric acid solutions
73at 25, 38, 50, 75, 84.5, and 95.6% H<SUB>2</SUB>SO<SUB>4</SUB>, by weight:</B></P>
74
75<P>Palmer K.F. and Dudley Williams, Optical constants of sulfuric acid;
76Application to the clouds of Venus?, <I>Appl.Opt.</I>, 1975, <B>14</B>,
77208-219. </P>
78
79<P><B>Real and imaginary indices of refraction of sulfuric acid solutions
80at 75 and 90% H<SUB>2</SUB>SO<SUB>4</SUB>, by weight, plus the standard
81deviations of the measurements. Real and imaginary indices of refraction
82of nitric acid solutions at 68% HNO<SUB>3</SUB>, by weight, plus the standard
83deviations of the measurements:</B></P>
84
85<P>Remsberg E.E., Lavery D., and Crawford B., Optical constants for sulfuric
86and nitric acids, <I>J.Chem. and Engin.Data </I>, 1974, <B>19</B>, 263-255.
87</P>
88
89<P><B>Theoretical equilibrium composition (weight percentage of H<SUB>2</SUB>SO<SUB>4</SUB>)
90of sulfuric acid solutions, given as a function of temperature and H<SUB>2</SUB>O
91vapour pressure:</B> </P>
92
93<P>Steele H.M., and Hamill P., Effects of temperature and humidity on the
94growth and optical properties of sulphuric acid-water droplets in the stratosphere,
95<I>J.Aerosol Sci</I>., 1981, <B>12</B>, 517-528.</P>
96
97<P><B>Sulfuric acid density (gm/cm<SUP>3</SUP>) values for solutions between
980 and 100% H<SUB>2</SUB>SO<SUB>4</SUB> (by weight) for temperatures between
990 and 60 C:</B></P>
100
101<P>Timmermans J., The physico-chemical constants of binary systems in concentrated
102solutions, Interscience, New York, (1960). </P>
103
104<P><B>Real and imaginary indices of refraction of H<SUB>2</SUB>O-ice, amorphous
105nitric acid solutions, and nitric acid hydrates: </B></P>
106
107<P>Toon O.B., Tolbert M.A., Koehler B.C., Middlebrook A.M., and Jordan
108J., The infrared optical constants of H<SUB>2</SUB>O-ice, amorphous acid
109solutions, and nitric acid hydrates, <I>J.Geophys.Res.</I> (in press 1994).
110</P>
111
112<hr>
113
114<CENTER><P><A HREF="geisa_update_gs03.html"><IMG SRC="/icons-geisa/prev.gif" BORDER=0 HEIGHT=50 WIDTH=91 ALIGN=ABSCENTER></A><B><FONT COLOR="#000080">MAIN&nbsp;PAGE</FONT></B></P></CENTER>
115
116<CENTER><P><A HREF="geisa_indupd_gs03.html"><IMG SRC="/icons-geisa/prev.gif" BORDER=0 HEIGHT=50 WIDTH=91></A><B><FONT COLOR="#000080">GEISA&nbsp;individual
117lines databank updates</FONT></B></P></CENTER>
118
119<CENTER><P><A HREF="geisa_crossupd_gs03.html"><IMG SRC="/icons-geisa/prev.gif" border=0 HEIGHT=50 WIDTH=91></A><B><FONT COLOR="#000080">GEISA
120absorption cross-sections databank updates</FONT></B></P></CENTER>
121
122</BODY>
123</HTML>
Note: See TracBrowser for help on using the repository browser.