Molecular spectroscopy Molecular spectroscopy
Guest | My Tasks
 Rus | Eng   
 |  Help
..Up
Tables for taking into account the Hartmann-Tran profiles in the H2O spectra calculations

Compact lookup tables for taking into account the Hartmann-Tran profiles in the H2O spectra calculations for the Mid-Latitude Summer Atmosphere

Each presented ASCII-file contains the cross-section spectra, calculated for one of the PT points of the Mid-Altitude Summer Atmospheric profile (MLS) [1] (see Table 1). The pressure P and temperature T used in the given calculation are shown in the filename.
For example, ‘P2p773-1_T235p2._10km’ means that calculation was performed at P=2.773E-1 atm and T=235.2 К (see Table 1 for 10km).

Table 1. Altitude Z, pressure P and temperature T used in calculations.
Z [km] P [atm] T [K] Download
0 1.000 294.0 P1p000-0_T294p0_0km
1 8.904E-1 290.0 P8p904-1_T290p0_1km
2 7.917E-1 285.0 P7p917-1_T285p0_2km
3 7.009E-1 279.0 P7p009-1_T279p0_3km
4 6.199E-1 273.0 P6p199-1_T273p0_4km
5 5.469E-1 267.1 P5p469-1_T267p1_5km
6 4.807E-1 261.0 P4p807-1_T261p0_6km
7 4.205E-1 254.7 P4p205-1_T254p7_7km
8 3.672E-1 248.2 P3p672-1_T248p2_8km
9 3.198E-1 241.7 P3p198-1_T241p7_9km
10 2.774E-1 235.2 P2p774-1_T235p2_10km
11 2.399E-1 228.8 P2p399-1_T228p8_11km
12 2.063E-1 222.3 P2p063-1_T222p3_12km
13 1.767E-1 216.9 P1p767-1_T216p9_13km
14 1.510E-1 215.8 P1p510-1_T215p8_14km
15 1.283E-1 215.8 P1p283-1_T215p8_15km
16 1.085E-1 215.8 P1p085-1_T215p8_16km
17 9.378E-2 215.8 P9_378-2_T215p8_17km
18 8.015E-2 216.0 P8p015-2_T216p0_18km
19 6.861E-2 217.0 P6p861-2_T217p0_19km
20 5.874E-2 218.2 P5p874-2_T218p2_20km
21 5.035E-2 219.4 P5p035-2_T219p4_21km
22 4.314E-2 220.6 P4p314-2_T220p6_22km
23 3.711E-2 221.8 P3p711-2_T221p8_23km
24 3.179E-2 223.0 P3p179-2_T223p0_24km
25 2.734E-2 224.2 P2p734-2_T224p2_25km
30 1.303E-2 234.2 P1p303-2_T234p2_30km
35 6.436E-3 245.3 P6p436-3_T245p3_35km
40 3.287E-3 257.5 P3p287-3_T257p5_40km
45 1.737E-3 269.7 P1p737-3_T269p7_45km
50 9.387E-4 276.2 P9p387-4_T276p2_50km
70 - - -
104 - - -

In each file there are four columns. The first one is the wavenumber grid (in cm-1). The second and third columns are the H2O cross-section spectra (in cm2) multiplied by factor 1020 (for convenience). These spectra have been calculated using the HITRAN-2016 [2] database taking into account only those spectral lines, which are equipped parameters for the Hartmann-Tran Profiles (HTP) [3] calculations. (In this database, out of 313,787 H2O lines, only 2655 lines are equipped with such parameters). Thus the second column is a sum of HTPs and the third one is a sum of usual Voigt profiles. The forth column is their difference. Table 2 demonstrate content of the above mentioned file as an example.

Table 2. Example: content of ‘P0.2773(-1) _T235.2.10km’ file.
Wavenumber (cm-1)    HTP (cm2)*1020    Voigt (cm2)*1020    (HTP-Voigt)*1020    
2690.31072 0.1385E-07 0.1353E-07 0.320E-09
2690.96608 0.2241E-07 0.2206E-07 0.350E-09
2691.62144 0.4260E-07 0.4221E-07 0.390E-09
2691.78528 0.5203E-07 0.5163E-07 0.400E-09
3999.67138 0.8674E-04 0.6769E-04 0.190E-04
3999.75330 0.8417E-04 0.6518E-04 0.190E-04
3999.83522 0.8185E-04 0.6293E-04 0.189E-04

The spectral range is the same in each file (2690-4000 cm-1). In the tables is used efficient nonuniform wavenumber grids for line profiles interpolations with a given accuracy (usually better than 1%). The grid points are condensed at the centers of the lines and become rare in the wings. It makes it possible to obtain essentially more compact files than those, which use uniform grids. But the grids are different in different files.

These files can be considered as demonstration of the spectral look-up tables (LUTs) for replacing direct line-by-line (LBL) calculations of molecular spectra in the forward remote sensing models for taking into account the non-Voigt line shapes. An efficient line-by-line technique of fast computing such as compact and precise LUTs plans to be published in near future.

These files can be considered as examples of compact “lookup tables” (LUTs) for taking into account the non-Voigt line shapes in forward line-by-line (LBL) models used in remote sensing. An effective methodology for calculating such LUTs is planned to be published in the near future.



INTAS grants 00-189, 03-51-3394, RFBR grants 02-07-90139, 05-07-90196, 08-07-00318