{"id":22,"date":"2023-06-07T19:41:08","date_gmt":"2023-06-07T19:41:08","guid":{"rendered":"https:\/\/itwg.ssec.wisc.edu\/rtsp\/?page_id=22"},"modified":"2023-07-21T16:04:04","modified_gmt":"2023-07-21T16:04:04","slug":"airs-fast-rt-model-comparisons","status":"publish","type":"page","link":"https:\/\/itwg.ssec.wisc.edu\/rtsp\/airs-fast-rt-model-comparisons\/","title":{"rendered":"AIRS fast RT model comparisons"},"content":{"rendered":"\n<h2 class=\"wp-block-heading\">Background<\/h2>\n\n\n\n<p>There are now several fast RT models in use for simulating AIRS radiances and so it was recommended at the workshop on Sounding from High Spectral Resolution Infrared Observations in Madison to initiate an intercomparison along the lines of the recent ATOVS comparison co-ordinated by Louis Garand. This page provides the specification for such a comparison of AIRS fast RT models\u00a0carried out as an ITWG activity and allows others to also take part if they wish and compare their model output with all the others which participated.\u00a0 The comparisons\u00a0are of the forward model calculations, level to space transmittances and the Jacobians with respect to T(p), q(p) and O<sub>3<\/sub>(p). The results from the comparison of 14 models (see below) are now available and a draft paper to JGR is available on request from\u00a0<a href=\"mailto:roger.saunders@metoffice.gov.uk\">Roger Saunders<\/a>\u00a0. The results submitted by each of the models are\u00a0available\u00a0<a href=\"https:\/\/itwg.ssec.wisc.edu\/rtsp\/airsrt-results\/\" data-type=\"page\" data-id=\"31\">here<\/a>\u00a0\u00a0and some plots of the results (from the JGR paper) are available\u00a0<a href=\"https:\/\/itwg.ssec.wisc.edu\/rtsp\/airsrt-plots\/\" data-type=\"page\" data-id=\"34\">here<\/a>.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Profiles and other input data to use<\/h2>\n\n\n\n<p>52 ECMWF model profiles on 101 AIRS levels available at: <a href=\"http:\/\/www.metoffice.com\/research\/interproj\/nwpsaf\/rtm\/\">http:\/\/www.metoffice.com\/research\/interproj\/nwpsaf\/rtm\/<\/a><\/p>\n\n\n\n<p>T (K), <em>q<\/em> (kg\/kg) specific humidity, O<sub>3<\/sub> (kg\/kg) and P<sub>s<\/sub> are specified. For the surface (e.g. skin temperature) the values (except P<sub>s<\/sub>) are specified in a separate file with a link on the same site as the profile data. To convert from specific concentration <em>q<\/em> in kg\/kg to volume mixing radio v in ppmv use the following equation:<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"213\" height=\"45\" src=\"https:\/\/itwg.ssec.wisc.edu\/rtsp\/wp-content\/uploads\/sites\/7\/2023\/06\/image.png\" alt=\"\" class=\"wp-image-23\" \/><\/figure>\n\n\n\n<p>where <em>M<sub>air<\/sub>\u00a0= 28.9644<\/em> and <em>M<sub>wv<\/sub><\/em>\u00a0= 18.01528 are the molecular weights of dry air and water vapour and <em>r<\/em> is their ratio <em>M<sub>wv<\/sub>\/M<sub>air<\/sub><\/em>= 0.62198. It is recommended to use software provided\u00a0<a href=\"https:\/\/itwg.ssec.wisc.edu\/rtsp\/wp-content\/uploads\/sites\/7\/2023\/06\/interp_f90.pdf\" data-type=\"attachment\" data-id=\"42\">here<\/a>\u00a0to interpolate profiles to other levels. For the surface assume a constant emissivity of 0.99 and the radiance of space to be zero. The profiles are assumed to be at night so there is no solar input. Line-by-line modellers should use their own default profiles for other gases or contact\u00a0<a href=\"mailto:roger.saunders@metoffice.com\">Roger Saunders<\/a>\u00a0for guidance. For the comparison with AIRS data the profiles and AIRS radiance data are at\u00a0\u00a0<a href=\"http:\/\/asl.umbc.edu\/pub\/hannon\/Roger\/TWP\/\">http:\/\/asl.umbc.edu\/pub\/hannon\/Roger\/TWP\/<\/a><\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Channels to simulate<\/h2>\n\n\n\n<p>For the forward model comparison results for all AIRS channels using 18 August 02 ISRF version 1 from Larrabee Strowe should be used. They are available from the following web site:\u00a0<a href=\"http:\/\/asl.umbc.edu\/pub\/airs\/srf\/\">http:\/\/asl.umbc.edu\/pub\/airs\/srf\/\u00a0<\/a>. The URL&#8217;s are:<br><a href=\"http:\/\/asl.umbc.edu\/pub\/airs\/srf\/srftables-020818v1.hdf\">http:\/\/asl.umbc.edu\/pub\/airs\/srf\/srftables-020818v1.hdf<\/a>\u00a0or\u00a0<a href=\"ftp:\/\/asl.umbc.edu\/pub\/airs\/srf\/srftables-020818v1.hdf\">ftp:\/\/asl.umbc.edu\/pub\/airs\/srf\/srftables-020818v1.hdf<\/a>\u00a0A document describing how to read this file is at\u00a0<a href=\"http:\/\/asl.umbc.edu\/pub\/airs\/srf\/srfhdf.pdf\">http:\/\/asl.umbc.edu\/pub\/airs\/srf\/srfhdf.pdf<\/a>\u00a0or\u00a0<a href=\"http:\/\/asl.umbc.edu\/pub\/airs\/srf\/srfhdf.html\">http:\/\/asl.umbc.edu\/pub\/airs\/srf\/srfhdf.html<\/a>\u00a0. If not all channels can be simulated then retain the same file format with 2378 channels but set those channels not simulated to have a brightness temperature of zero.<\/p>\n\n\n\n<p>For level to space transmittance and Jacobians just 20 channels as defined in the table below should be submitted in order to make the file sizes manageable. The columns with a X in denote those elements of the state vector where transmittances and Jacobians will be compared but for simplicity it is suggested users submit results for all profile elements. In fact the temperature Jacobians for the water vapour channels are still of interest.<\/p>\n\n\n\n<figure class=\"wp-block-table\"><table><tbody><tr><td><strong>AIRS channel number<\/strong><\/td><td><strong>Frequency<\/strong><br><strong>(cm-1)<\/strong><\/td><td><strong>Level to space transmittance<\/strong><\/td><td><strong>Temperature jacobian<\/strong><\/td><td><strong>Water vapour jacobian<\/strong><\/td><td><strong>Ozone jacobian<\/strong><\/td><\/tr><tr><td>71<\/td><td>666.7<\/td><td>X<\/td><td>X<\/td><td>&nbsp;<\/td><td>&nbsp;<\/td><\/tr><tr><td>77<\/td><td>668.2<\/td><td>X<\/td><td>X<\/td><td>&nbsp;<\/td><td>&nbsp;<\/td><\/tr><tr><td>305<\/td><td>737.1<\/td><td>X<\/td><td>X<\/td><td>&nbsp;<\/td><td>&nbsp;<\/td><\/tr><tr><td>453<\/td><td>793.1<\/td><td>X<\/td><td>X<\/td><td>X<\/td><td>&nbsp;<\/td><\/tr><tr><td>672<\/td><td>871.2<\/td><td>X<\/td><td>X<\/td><td>X<\/td><td>&nbsp;<\/td><\/tr><tr><td>787<\/td><td>917.2<\/td><td>X<\/td><td>X<\/td><td>&nbsp;<\/td><td>&nbsp;<\/td><\/tr><tr><td>1021<\/td><td>1009.2<\/td><td>X<\/td><td>X<\/td><td>&nbsp;<\/td><td>X<\/td><\/tr><tr><td>1090<\/td><td>1040.1<\/td><td>X<\/td><td>&nbsp;<\/td><td>&nbsp;<\/td><td>X<\/td><\/tr><tr><td>1142<\/td><td>1074.3<\/td><td>X<\/td><td>&nbsp;<\/td><td>X<\/td><td>&nbsp;<\/td><\/tr><tr><td>1437<\/td><td>1323.8<\/td><td>X<\/td><td>&nbsp;<\/td><td>X<\/td><td>&nbsp;<\/td><\/tr><tr><td>1449<\/td><td>1330.8<\/td><td>X<\/td><td>&nbsp;<\/td><td>X<\/td><td>&nbsp;<\/td><\/tr><tr><td>1627<\/td><td>1427.1<\/td><td>X<\/td><td>&nbsp;<\/td><td>X<\/td><td>&nbsp;<\/td><\/tr><tr><td>1766<\/td><td>1544.3<\/td><td>X<\/td><td>&nbsp;<\/td><td>X<\/td><td>&nbsp;<\/td><\/tr><tr><td>1794<\/td><td>1563.5<\/td><td>X<\/td><td>&nbsp;<\/td><td>X<\/td><td>&nbsp;<\/td><\/tr><tr><td>1812<\/td><td>1576.1<\/td><td>X<\/td><td>&nbsp;<\/td><td>X<\/td><td>&nbsp;<\/td><\/tr><tr><td>1917<\/td><td>2229.3<\/td><td>X<\/td><td>X<\/td><td>&nbsp;<\/td><td>&nbsp;<\/td><\/tr><tr><td>1958<\/td><td>2268.7<\/td><td>X<\/td><td>X<\/td><td>&nbsp;<\/td><td>&nbsp;<\/td><\/tr><tr><td>1995<\/td><td>2305.5<\/td><td>X<\/td><td>X<\/td><td>&nbsp;<\/td><td>&nbsp;<\/td><\/tr><tr><td>2107<\/td><td>2385.9<\/td><td>X<\/td><td>X<\/td><td>&nbsp;<\/td><td>&nbsp;<\/td><\/tr><tr><td>2197<\/td><td>2500.3<\/td><td>X<\/td><td>X<\/td><td><\/td><td><\/td><\/tr><\/tbody><\/table><figcaption class=\"wp-element-caption\"><strong><em>Table 1 Channels for Jacobian comparison<\/em><\/strong>.<\/figcaption><\/figure>\n\n\n\n<h2 class=\"wp-block-heading\">Outputs required<\/h2>\n\n\n\n<p>See table below. For forward model runs 3 files are required for nadir, 45 deg and 60 deg local zenith angle from the surface. A plane parallel atmosphere is assumed for all calculations.<\/p>\n\n\n\n<figure class=\"wp-block-table\"><table><tbody><tr><td><strong>dParameter<\/strong><\/td><td><strong>Units<\/strong><\/td><td><strong>Dimensions<\/strong><\/td><td><strong>Filenames<\/strong><\/td><td><strong>Status<\/strong><\/td><\/tr><tr><td>TOA BT<\/td><td>K<\/td><td>2378&#215;52<\/td><td>Fwd_nadir.dat<br>Fwd_45deg.dat<br>Fwd_60deg.dat<\/td><td>Mandatory for at least a channel subset.<\/td><\/tr><tr><td>&nbsp;dBT\/dT<\/td><td>K\/K<\/td><td>20xjx52<\/td><td rowspan=\"4\">Jac_nadir.dat<br>Jac_45deg.dat<br>Jac_60deg.dat<\/td><td>Optional<\/td><\/tr><tr><td>dBT\/dq<\/td><td>K\/(kg\/kg)<\/td><td>20xjx52<\/td><td>Optional<\/td><\/tr><tr><td>dBT\/dO3<\/td><td>K\/(kg\/kg)<\/td><td>20xjx52<\/td><td>Optional<\/td><\/tr><tr><td>Level to space transmittance<\/td><td>0-1<\/td><td>20xjx52<\/td><td>Optional<\/td><\/tr><\/tbody><\/table><figcaption class=\"wp-element-caption\"><strong><em>Table 2 Output data required for comparison participants<\/em><\/strong><\/figcaption><\/figure>\n\n\n\n<p>For the Jacobians the temperature perturbation is +1K, for the specific humidity and ozone the perturbation is -1% of the layer mean concentration. For finite difference Jacobians it should be +\/- 0.5K and +\/- 0.5% of the layer mean concentration at the pressure levels used. If outputs are not on 101 levels provide on your own\u00a0<em>j<\/em>\u00a0levels and let the co-ordinator interpolate to the 101 levels. File formats are in ascii (see examples for RTTOV-7\u00a0<a href=\"https:\/\/cimss.ssec.wisc.edu\/itwg\/groups\/rtwg\/fwd_nadir.lst\">here<\/a>\u00a0for forward model results and\u00a0<a href=\"https:\/\/cimss.ssec.wisc.edu\/itwg\/groups\/rtwg\/jac_nadir.lst\">here<\/a>\u00a0for jacobian results). The FORTRAN code to write out the fwd files is\u00a0<a href=\"https:\/\/cimss.ssec.wisc.edu\/itwg\/groups\/rtwg\/fwd_format.f90\">here<\/a>\u00a0and for Jacobians is\u00a0<a href=\"https:\/\/cimss.ssec.wisc.edu\/itwg\/groups\/rtwg\/jac_format.f90\">here<\/a>. A record of the times taken to run the forward model computation for all channels and profiles and the Jacobians for 20 channels and all profiles should be given by email. When the results are compiled the details of the line by line model and spectroscopic datasets on which the fast model is based will also be required.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Current participants and status<\/h2>\n\n\n\n<figure class=\"wp-block-table\"><table><tbody><tr><td><\/td><td><\/td><td><\/td><td><\/td><td><\/td><\/tr><tr><td>Model\u00a0\u00a0name<br>Reference<\/td><td>Base model\u00a0\u00a0\u00a0spectroscopy<br>w.v. continuum<br>line mixing<\/td><td>Participant<\/td><td>Results submitted<br>Transmittances\/Jacobian<\/td><td>Method<\/td><\/tr><tr><td>RTTOV-7<br><em>Saunders et al 1999<\/em><\/td><td>GENLN2v2<br>Hitran-96<br>CKD2.1<br><em>Strow et al 1994<\/em><\/td><td>R. Saunders,<br>Met Office<\/td><td>Yes\/<br>Analytic<\/td><td>Regression<\/td><\/tr><tr><td>RTTOV-8<br><em>Saunders et al 1999<\/em><\/td><td>kCarta (1.11)<sup>1<\/sup><br>Hitran-2004Modified<br>MTCKD 1.0<br><em>DeSouza-Machado et al 1999<\/em><\/td><td>R. Saunders,<br>P. Brunel<br>Met Office<\/td><td>Yes\/<br>Analytic<\/td><td>Regression<\/td><\/tr><tr><td>Optran v7<br><em>Xiong and McMillin et. al. 2005, McMillin et al 2005<\/em><\/td><td>LBLRTM v7.04<br>HITRAN-2000<br>MTCKD 1.0<br><em>Hoke et. al. 1989<\/em><\/td><td>Y. Han, NESDIS<\/td><td>Yes\/<br>Analytic<\/td><td>Regression<\/td><\/tr><tr><td>OSS<br><em>Moncet et al 2004<\/em><\/td><td>LBLRTMV8.3<br>HITRAN-2000<br>MTCKD 1.0<br><em>Hoke et. al. 1989<\/em><\/td><td>J-L. Moncet,&nbsp;&nbsp;G. Uymin, AER<\/td><td>None\/<br>Analytic<\/td><td>Pre-computed LUT<\/td><\/tr><tr><td>\u03c3-IASI<em>Amato et. al. 2002<\/em><\/td><td>LBLRTMV8.1<br>HITRAN-2000<br>MTCKD 1.0<br><em>Hoke et. al. 1989<\/em><\/td><td>G. Masiello,C. Serio,DIFA\u00ad, UniBas<\/td><td>Yes\/<br>Analytic<\/td><td>Pre-computed LUT<\/td><\/tr><tr><td>Gastropod 0.3.0<em>Sherlock et. al. 2003<\/em><\/td><td>kCarta 2000<sup>1<\/sup><br>Hitran-1998<sup>2<\/sup><br>CKD2.4<br><em>Strow et al 2003<\/em><\/td><td>V. Sherlock, NIWA<\/td><td>Yes\/<br>Analytic<\/td><td>Regression<\/td><\/tr><tr><td>SARTAv 1.05<em>Strow et. al. 2003<\/em><\/td><td>kCarta (1.07)<sup>1<\/sup><br>Hitran-2000<br>Modified MTCKD 1.0<br><em>DeSouza-Machado et al 1999<\/em><\/td><td>S. Hannon,L. Strow, UMBC<\/td><td>None\/<br>None<\/td><td>Regression<\/td><\/tr><tr><td>PCRTM<em>Liu et. al 2006<\/em><\/td><td>LBLRTM v8.3<br>Hitran-2000<br>MTCKD 1.0<br><em>Hoke et. al. 1989<\/em><\/td><td>Xu Liu,NASA, LaRC<\/td><td>Yes\/<br>Analytical<\/td><td>LUT\/<br>Regression<\/td><\/tr><\/tbody><\/table><figcaption class=\"wp-element-caption\"><em>Table 3. Fast models which participated in the comparison<\/em><\/figcaption><\/figure>\n\n\n\n<p><sup>1<\/sup>kCarta is described in Strow\u00a0<em>et. al.\u00a0<\/em>(1998)<\/p>\n\n\n\n<p><sup>2<\/sup>includes the Toth H<sub>2<\/sub>O lines<em>&nbsp;&nbsp;&nbsp; &nbsp;&nbsp;&nbsp; &nbsp;&nbsp;&nbsp; &nbsp;&nbsp;&nbsp;&nbsp;<\/em><\/p>\n\n\n\n<figure class=\"wp-block-table\"><table><tbody><tr><td>Model\u00a0\u00a0name<br>Reference<\/td><td>Base model\u00a0spectroscopy<br>w.v. continuum<br>line mixing<\/td><td>Participant<\/td><td>Results submitted<br>Transmittances\/Jacobian<\/td><td>Method<\/td><\/tr><tr><td>RFM<br><em>http:\/\/www.atm.ox.ac.uk\/RFM<\/em><\/td><td>GENLN2<br>HITRAN-2000<br>CKD2.4<br><em>Strow et al 1994<\/em><\/td><td>N. Bormann, ECMWF<\/td><td>Yes\/<br>Finite diff<\/td><td>&nbsp;Full LbL computation<\/td><\/tr><tr><td>LBLRTM v8.3\u00a0<br><em>Clough et. al. 1992<\/em><\/td><td>HITRAN-2000<br>MTCKD 1.0<br><em>Hoke et al., 1989<\/em><\/td><td>J-L. Moncet, AER<\/td><td>None\/<br>Finite diff<\/td><td>&nbsp;Full LbL computation<\/td><\/tr><tr><td>ARTS 1.0.136<br><em>Buehler et. al. 2005<\/em><\/td><td>HITRAN-2003<br>MTCKD 1.0<br>None<\/td><td>A. von Engeln,<br>Bremen<\/td><td>None\/<br>None<\/td><td>&nbsp;Full LbL computation<\/td><\/tr><tr><td>4A\u00a0<br><em>Scott and Ch\u00e9din, 1981 and http:\/\/www.noveltis.net\/4AOP\/<\/em><\/td><td>STRANSAC<br>GEISA 2001<br><em>Rodriguez et al 1999<\/em><\/td><td>S. Heilliette, LMD<\/td><td>Yes\/<br>Analytic<\/td><td>Pre-computed LUT<\/td><\/tr><tr><td>FLBL-3<br><em>Turner, 1995<\/em><\/td><td>HITRAN-2001<br>CKD2.4<br><em>Strow et al 1998<\/em><\/td><td>D.S. Turner,<br>MSC<\/td><td>Yes\/<br>Analytic<\/td><td>Pre-computed LUT<\/td><\/tr><tr><td>HARTCODE<br><em>Miskolczi et al 1989<\/em><\/td><td>HITRAN-2000<br>CKD2.4<br><em>Rodriguez et al 1999<\/em><\/td><td>F. Miskolczi,<br>NASA, LaRC<\/td><td>None\/<br>None<\/td><td>Full LbL computation<\/td><\/tr><\/tbody><\/table><figcaption class=\"wp-element-caption\"><em>Table 4. Line-by-line models which participated in the comparison.<\/em><\/figcaption><\/figure>\n\n\n\n<h2 class=\"wp-block-heading\">Timetable<\/h2>\n\n\n\n<p>June 03 &#8211; Announce to ITWG<br>Sep 03 &#8211; Collect initial results<br>Oct 03 &#8211; Present preliminary results at ITSC-13<br>Jun 05 &#8211; Presented final results at ITSC-14<br>Jan 06 &#8211; Paper submitted to JGR (Atmospheres)<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Results<\/h2>\n\n\n\n<p>The results submitted by each of the models are available\u00a0<a href=\"https:\/\/itwg.ssec.wisc.edu\/rtsp\/airsrt-results\/\" data-type=\"page\" data-id=\"31\">here<\/a>. Some plots summarising an analysis of the results are also presented\u00a0<a href=\"https:\/\/itwg.ssec.wisc.edu\/rtsp\/airsrt-plots\/\" data-type=\"page\" data-id=\"34\">here<\/a>.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Background There are now several fast RT models in use for simulating AIRS radiances and so it was recommended at the workshop on Sounding from High Spectral Resolution Infrared Observations in Madison to initiate an intercomparison along the lines of the recent ATOVS comparison co-ordinated by Louis Garand. This page provides the specification for such [&hellip;]<\/p>\n","protected":false},"author":3,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_acf_changed":false,"footnotes":""},"class_list":["post-22","page","type-page","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/itwg.ssec.wisc.edu\/rtsp\/wp-json\/wp\/v2\/pages\/22","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/itwg.ssec.wisc.edu\/rtsp\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/itwg.ssec.wisc.edu\/rtsp\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/itwg.ssec.wisc.edu\/rtsp\/wp-json\/wp\/v2\/users\/3"}],"replies":[{"embeddable":true,"href":"https:\/\/itwg.ssec.wisc.edu\/rtsp\/wp-json\/wp\/v2\/comments?post=22"}],"version-history":[{"count":7,"href":"https:\/\/itwg.ssec.wisc.edu\/rtsp\/wp-json\/wp\/v2\/pages\/22\/revisions"}],"predecessor-version":[{"id":45,"href":"https:\/\/itwg.ssec.wisc.edu\/rtsp\/wp-json\/wp\/v2\/pages\/22\/revisions\/45"}],"wp:attachment":[{"href":"https:\/\/itwg.ssec.wisc.edu\/rtsp\/wp-json\/wp\/v2\/media?parent=22"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}