Coupling photochemistry with haze formation in Titan's atmosphere, Part II: Results and validation with Cassini/Huygens data
The new one-dimensional radiative–convective/photochemical/microphysical model described in Part I is applied to the study of Titan's atmospheric processes that lead to haze formation. Our model generates the haze structure from the gaseous species photochemistry. Model results are presented fo...
Gespeichert in:
Veröffentlicht in: | Planetary and space science 2008, Vol.56 (1), p.67-99 |
---|---|
Hauptverfasser: | , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | 99 |
---|---|
container_issue | 1 |
container_start_page | 67 |
container_title | Planetary and space science |
container_volume | 56 |
creator | Lavvas, P.P. Coustenis, A. Vardavas, I.M. |
description | The new one-dimensional radiative–convective/photochemical/microphysical model described in Part I is applied to the study of Titan's atmospheric processes that lead to haze formation. Our model generates the haze structure from the gaseous species photochemistry. Model results are presented for the species vertical concentration profiles, haze formation and its radiative properties, vertical temperature/density profiles and geometric albedo. These are validated against Cassini/Huygens observations and other ground-based and space-borne measurements. The model reproduces well most of the latest measurements from the Cassini/Huygens instruments for the chemical composition of Titan's atmosphere and the vertical profiles of the observed species. For the haze production we have included pathways that are based on pure hydrocarbons, pure nitriles and hydrocarbon/nitrile copolymers. From these, the nitrile and copolymer pathways provide the stronger contribution, in agreement with the results from the ACP instrument, which support the incorporation of nitrogen in the pyrolized haze structures. Our haze model reveals a new second major peak in the vertical profile of haze production rate between 500 and 900
km. This peak is produced by the copolymer family used and has important ramifications for the vertical atmospheric temperature profile and geometric albedo. In particular, the existence of this second peak determines the vertical profile of haze extinction. Our model results have been compared with the DISR retrieved haze extinction profiles and are found to be in very good agreement. We have also incorporated in our model heterogeneous chemistry on the haze particles that converts atomic hydrogen to molecular hydrogen. The resultant H
2 profile is closer to the INMS measurements, while the vertical profile of the diacetylene formed is found to be closer to that of the CIRS profile when this heterogenous chemistry is included. |
doi_str_mv | 10.1016/j.pss.2007.05.027 |
format | Article |
fullrecord | <record><control><sourceid>proquest_hal_p</sourceid><recordid>TN_cdi_hal_primary_oai_HAL_hal_03786076v1</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0032063307002292</els_id><sourcerecordid>19474952</sourcerecordid><originalsourceid>FETCH-LOGICAL-c362t-9bcad2ab101308d9d02b61c28e4cb0fe455f4206b6e93d046df8e1c1030b16cb3</originalsourceid><addsrcrecordid>eNp9kVGr1DAQhYsouF79Ab7lSRFs7yRp01afLou6CwuKXJ9Dmk5vs3STmqQrK_54s1Z89Glg5pwDZ74se0mhoEDF7bGYQygYQF1AVQCrH2Ub2tQ8r6BpHmcbAM5yEJw_zZ6FcAQAIVi9yX5t3TJPxj6QeXTR6RFPJkR_IT9MHMmofiIZnD-paJwlxpJ7E5V9HYiKJxfmET2-JV-Uj2S_f0e-YlimmI62J2c1mX61_YnaqhCMNbe75fKANpB0U8-zJ4OaAr74O2-ybx8_3G93-eHzp_327pBrLljM206rnqkuFeXQ9G0PrBNUswZL3cGAZVUNJQPRCWx5D6XohwappsCho0J3_CZ7s-aOapKzNyflL9IpI3d3B3ndAa8bAbU406R9tWpn774vGKJMD9E4TcqiW4KkbVmXbcWSkK5C7V0IHod_yRTklYk8ysREXplIqGRikjzvVw-mtmeDXgZt0GrsjUcdZe_Mf9y_AfspleU</addsrcrecordid><sourcetype>Open Access Repository</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>19474952</pqid></control><display><type>article</type><title>Coupling photochemistry with haze formation in Titan's atmosphere, Part II: Results and validation with Cassini/Huygens data</title><source>Elsevier ScienceDirect Journals</source><creator>Lavvas, P.P. ; Coustenis, A. ; Vardavas, I.M.</creator><creatorcontrib>Lavvas, P.P. ; Coustenis, A. ; Vardavas, I.M.</creatorcontrib><description>The new one-dimensional radiative–convective/photochemical/microphysical model described in Part I is applied to the study of Titan's atmospheric processes that lead to haze formation. Our model generates the haze structure from the gaseous species photochemistry. Model results are presented for the species vertical concentration profiles, haze formation and its radiative properties, vertical temperature/density profiles and geometric albedo. These are validated against Cassini/Huygens observations and other ground-based and space-borne measurements. The model reproduces well most of the latest measurements from the Cassini/Huygens instruments for the chemical composition of Titan's atmosphere and the vertical profiles of the observed species. For the haze production we have included pathways that are based on pure hydrocarbons, pure nitriles and hydrocarbon/nitrile copolymers. From these, the nitrile and copolymer pathways provide the stronger contribution, in agreement with the results from the ACP instrument, which support the incorporation of nitrogen in the pyrolized haze structures. Our haze model reveals a new second major peak in the vertical profile of haze production rate between 500 and 900
km. This peak is produced by the copolymer family used and has important ramifications for the vertical atmospheric temperature profile and geometric albedo. In particular, the existence of this second peak determines the vertical profile of haze extinction. Our model results have been compared with the DISR retrieved haze extinction profiles and are found to be in very good agreement. We have also incorporated in our model heterogeneous chemistry on the haze particles that converts atomic hydrogen to molecular hydrogen. The resultant H
2 profile is closer to the INMS measurements, while the vertical profile of the diacetylene formed is found to be closer to that of the CIRS profile when this heterogenous chemistry is included.</description><identifier>ISSN: 0032-0633</identifier><identifier>EISSN: 1873-5088</identifier><identifier>DOI: 10.1016/j.pss.2007.05.027</identifier><language>eng</language><publisher>Elsevier Ltd</publisher><subject>Astrophysics ; Atmosphere structure and composition ; Haze ; Physics ; Temperature ; Titan</subject><ispartof>Planetary and space science, 2008, Vol.56 (1), p.67-99</ispartof><rights>2007 Elsevier Ltd</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c362t-9bcad2ab101308d9d02b61c28e4cb0fe455f4206b6e93d046df8e1c1030b16cb3</citedby><cites>FETCH-LOGICAL-c362t-9bcad2ab101308d9d02b61c28e4cb0fe455f4206b6e93d046df8e1c1030b16cb3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0032063307002292$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>230,314,776,780,881,3537,4010,27900,27901,27902,65306</link.rule.ids><backlink>$$Uhttps://hal.science/hal-03786076$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Lavvas, P.P.</creatorcontrib><creatorcontrib>Coustenis, A.</creatorcontrib><creatorcontrib>Vardavas, I.M.</creatorcontrib><title>Coupling photochemistry with haze formation in Titan's atmosphere, Part II: Results and validation with Cassini/Huygens data</title><title>Planetary and space science</title><description>The new one-dimensional radiative–convective/photochemical/microphysical model described in Part I is applied to the study of Titan's atmospheric processes that lead to haze formation. Our model generates the haze structure from the gaseous species photochemistry. Model results are presented for the species vertical concentration profiles, haze formation and its radiative properties, vertical temperature/density profiles and geometric albedo. These are validated against Cassini/Huygens observations and other ground-based and space-borne measurements. The model reproduces well most of the latest measurements from the Cassini/Huygens instruments for the chemical composition of Titan's atmosphere and the vertical profiles of the observed species. For the haze production we have included pathways that are based on pure hydrocarbons, pure nitriles and hydrocarbon/nitrile copolymers. From these, the nitrile and copolymer pathways provide the stronger contribution, in agreement with the results from the ACP instrument, which support the incorporation of nitrogen in the pyrolized haze structures. Our haze model reveals a new second major peak in the vertical profile of haze production rate between 500 and 900
km. This peak is produced by the copolymer family used and has important ramifications for the vertical atmospheric temperature profile and geometric albedo. In particular, the existence of this second peak determines the vertical profile of haze extinction. Our model results have been compared with the DISR retrieved haze extinction profiles and are found to be in very good agreement. We have also incorporated in our model heterogeneous chemistry on the haze particles that converts atomic hydrogen to molecular hydrogen. The resultant H
2 profile is closer to the INMS measurements, while the vertical profile of the diacetylene formed is found to be closer to that of the CIRS profile when this heterogenous chemistry is included.</description><subject>Astrophysics</subject><subject>Atmosphere structure and composition</subject><subject>Haze</subject><subject>Physics</subject><subject>Temperature</subject><subject>Titan</subject><issn>0032-0633</issn><issn>1873-5088</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2008</creationdate><recordtype>article</recordtype><recordid>eNp9kVGr1DAQhYsouF79Ab7lSRFs7yRp01afLou6CwuKXJ9Dmk5vs3STmqQrK_54s1Z89Glg5pwDZ74se0mhoEDF7bGYQygYQF1AVQCrH2Ub2tQ8r6BpHmcbAM5yEJw_zZ6FcAQAIVi9yX5t3TJPxj6QeXTR6RFPJkR_IT9MHMmofiIZnD-paJwlxpJ7E5V9HYiKJxfmET2-JV-Uj2S_f0e-YlimmI62J2c1mX61_YnaqhCMNbe75fKANpB0U8-zJ4OaAr74O2-ybx8_3G93-eHzp_327pBrLljM206rnqkuFeXQ9G0PrBNUswZL3cGAZVUNJQPRCWx5D6XohwappsCho0J3_CZ7s-aOapKzNyflL9IpI3d3B3ndAa8bAbU406R9tWpn774vGKJMD9E4TcqiW4KkbVmXbcWSkK5C7V0IHod_yRTklYk8ysREXplIqGRikjzvVw-mtmeDXgZt0GrsjUcdZe_Mf9y_AfspleU</recordid><startdate>2008</startdate><enddate>2008</enddate><creator>Lavvas, P.P.</creator><creator>Coustenis, A.</creator><creator>Vardavas, I.M.</creator><general>Elsevier Ltd</general><general>Elsevier</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>KL.</scope><scope>1XC</scope></search><sort><creationdate>2008</creationdate><title>Coupling photochemistry with haze formation in Titan's atmosphere, Part II: Results and validation with Cassini/Huygens data</title><author>Lavvas, P.P. ; Coustenis, A. ; Vardavas, I.M.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c362t-9bcad2ab101308d9d02b61c28e4cb0fe455f4206b6e93d046df8e1c1030b16cb3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2008</creationdate><topic>Astrophysics</topic><topic>Atmosphere structure and composition</topic><topic>Haze</topic><topic>Physics</topic><topic>Temperature</topic><topic>Titan</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Lavvas, P.P.</creatorcontrib><creatorcontrib>Coustenis, A.</creatorcontrib><creatorcontrib>Vardavas, I.M.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Hyper Article en Ligne (HAL)</collection><jtitle>Planetary and space science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Lavvas, P.P.</au><au>Coustenis, A.</au><au>Vardavas, I.M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Coupling photochemistry with haze formation in Titan's atmosphere, Part II: Results and validation with Cassini/Huygens data</atitle><jtitle>Planetary and space science</jtitle><date>2008</date><risdate>2008</risdate><volume>56</volume><issue>1</issue><spage>67</spage><epage>99</epage><pages>67-99</pages><issn>0032-0633</issn><eissn>1873-5088</eissn><abstract>The new one-dimensional radiative–convective/photochemical/microphysical model described in Part I is applied to the study of Titan's atmospheric processes that lead to haze formation. Our model generates the haze structure from the gaseous species photochemistry. Model results are presented for the species vertical concentration profiles, haze formation and its radiative properties, vertical temperature/density profiles and geometric albedo. These are validated against Cassini/Huygens observations and other ground-based and space-borne measurements. The model reproduces well most of the latest measurements from the Cassini/Huygens instruments for the chemical composition of Titan's atmosphere and the vertical profiles of the observed species. For the haze production we have included pathways that are based on pure hydrocarbons, pure nitriles and hydrocarbon/nitrile copolymers. From these, the nitrile and copolymer pathways provide the stronger contribution, in agreement with the results from the ACP instrument, which support the incorporation of nitrogen in the pyrolized haze structures. Our haze model reveals a new second major peak in the vertical profile of haze production rate between 500 and 900
km. This peak is produced by the copolymer family used and has important ramifications for the vertical atmospheric temperature profile and geometric albedo. In particular, the existence of this second peak determines the vertical profile of haze extinction. Our model results have been compared with the DISR retrieved haze extinction profiles and are found to be in very good agreement. We have also incorporated in our model heterogeneous chemistry on the haze particles that converts atomic hydrogen to molecular hydrogen. The resultant H
2 profile is closer to the INMS measurements, while the vertical profile of the diacetylene formed is found to be closer to that of the CIRS profile when this heterogenous chemistry is included.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/j.pss.2007.05.027</doi><tpages>33</tpages></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0032-0633 |
ispartof | Planetary and space science, 2008, Vol.56 (1), p.67-99 |
issn | 0032-0633 1873-5088 |
language | eng |
recordid | cdi_hal_primary_oai_HAL_hal_03786076v1 |
source | Elsevier ScienceDirect Journals |
subjects | Astrophysics Atmosphere structure and composition Haze Physics Temperature Titan |
title | Coupling photochemistry with haze formation in Titan's atmosphere, Part II: Results and validation with Cassini/Huygens data |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-11T13%3A15%3A23IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_hal_p&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Coupling%20photochemistry%20with%20haze%20formation%20in%20Titan's%20atmosphere,%20Part%20II:%20Results%20and%20validation%20with%20Cassini/Huygens%20data&rft.jtitle=Planetary%20and%20space%20science&rft.au=Lavvas,%20P.P.&rft.date=2008&rft.volume=56&rft.issue=1&rft.spage=67&rft.epage=99&rft.pages=67-99&rft.issn=0032-0633&rft.eissn=1873-5088&rft_id=info:doi/10.1016/j.pss.2007.05.027&rft_dat=%3Cproquest_hal_p%3E19474952%3C/proquest_hal_p%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=19474952&rft_id=info:pmid/&rft_els_id=S0032063307002292&rfr_iscdi=true |