Near micron-sized cirrus cloud particles in high-resolution infrared spectra: An orographic case study
The high‐resolution spectra of the Atmospheric Infrared Sounder (AIRS) provide a global view of small‐ particle‐dominated cirrus clouds, and they exist over much larger spatial extents than seen in previous aircraft campaigns. As shown by simulations using a plane‐parallel scattering radiative trans...
Gespeichert in:
| Veröffentlicht in: | Geophysical research letters 2003-04, Vol.30 (8), p.24.1-n/a |
|---|---|
| Hauptverfasser: | , , , , , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | n/a |
|---|---|
| container_issue | 8 |
| container_start_page | 24.1 |
| container_title | Geophysical research letters |
| container_volume | 30 |
| creator | Kahn, Brian H. Eldering, Annmarie Clough, Shepard A. Fetzer, Eric J. Fishbein, Evan Gunson, Michael R. Lee, Sung-Yung Lester, Peter F. Realmuto, Vincent J. |
| description | The high‐resolution spectra of the Atmospheric Infrared Sounder (AIRS) provide a global view of small‐ particle‐dominated cirrus clouds, and they exist over much larger spatial extents than seen in previous aircraft campaigns. As shown by simulations using a plane‐parallel scattering radiative transfer (RT) model and realistic ice particle shapes, the shape of the radiance spectra in the atmospheric windows is uniquely influenced by small ice crystals. Minima in the brightness temperature (BT) spectra between 800 to 850 cm−1 are seen for ice particles smaller than 3 μm in the RT simulations and AIRS spectra. A case study of an orographic cirrus cloud observed on October 2, 2002, over the central Andes of South America is presented with spectral BT differences up to 63K between 998 and 811 cm−1. |
| doi_str_mv | 10.1029/2003GL016909 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_27914472</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>27914472</sourcerecordid><originalsourceid>FETCH-LOGICAL-c3757-1f5f384e1a62f4a45654dc80661bb32b5373c22974a0ca2a5dd3f2272168b8483</originalsourceid><addsrcrecordid>eNp9kE1P3DAQhq0KJBbaW3-AL-2JgL9ix9wQggVpRUUF4mjNOg7rNpuknkSw_fUYLQJOnGY08zyvNEPId86OOBP2WDAm5wvGtWX2C5lxq1RRMWZ2yIwxm3th9B7ZR_zDMskkn5HmOkCi6-hT3xUY_4ea-pjShNS3_VTTAdIYfRuQxo6u4sOqSAH7dhpj3-VRkyBlBYfgxwQn9LSjfeofEgyr6KkHDBTHqd58JbsNtBi-vdYDcndxfnt2WSx-za_OTheFl6Y0BW_KRlYqcNCiUaBKXaraV0xrvlxKsSylkV4IaxQwDwLKupaNEEZwXS0rVckD8nObO6T-3xRwdOuIPrQtdKGf0AljuVJGZPBwC-bDEVNo3JDiGtLGceZenuk-PjPjP15zAT20-ezOR3x3lBVWVTxzYss9xjZsPs10898Lro02WSq2UsQxPL1JkP66vDWlu7-eO6sFv7-R0l3IZ8IykWU</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>27914472</pqid></control><display><type>article</type><title>Near micron-sized cirrus cloud particles in high-resolution infrared spectra: An orographic case study</title><source>Wiley-Blackwell AGU Digital Library</source><source>Wiley Online Library Journals Frontfile Complete</source><source>Wiley Online Library Free Content</source><source>Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals</source><creator>Kahn, Brian H. ; Eldering, Annmarie ; Clough, Shepard A. ; Fetzer, Eric J. ; Fishbein, Evan ; Gunson, Michael R. ; Lee, Sung-Yung ; Lester, Peter F. ; Realmuto, Vincent J.</creator><creatorcontrib>Kahn, Brian H. ; Eldering, Annmarie ; Clough, Shepard A. ; Fetzer, Eric J. ; Fishbein, Evan ; Gunson, Michael R. ; Lee, Sung-Yung ; Lester, Peter F. ; Realmuto, Vincent J.</creatorcontrib><description>The high‐resolution spectra of the Atmospheric Infrared Sounder (AIRS) provide a global view of small‐ particle‐dominated cirrus clouds, and they exist over much larger spatial extents than seen in previous aircraft campaigns. As shown by simulations using a plane‐parallel scattering radiative transfer (RT) model and realistic ice particle shapes, the shape of the radiance spectra in the atmospheric windows is uniquely influenced by small ice crystals. Minima in the brightness temperature (BT) spectra between 800 to 850 cm−1 are seen for ice particles smaller than 3 μm in the RT simulations and AIRS spectra. A case study of an orographic cirrus cloud observed on October 2, 2002, over the central Andes of South America is presented with spectral BT differences up to 63K between 998 and 811 cm−1.</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/2003GL016909</identifier><identifier>CODEN: GPRLAJ</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>Cloud physics ; Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Meteorology</subject><ispartof>Geophysical research letters, 2003-04, Vol.30 (8), p.24.1-n/a</ispartof><rights>Copyright 2003 by the American Geophysical Union.</rights><rights>2003 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3757-1f5f384e1a62f4a45654dc80661bb32b5373c22974a0ca2a5dd3f2272168b8483</citedby><cites>FETCH-LOGICAL-c3757-1f5f384e1a62f4a45654dc80661bb32b5373c22974a0ca2a5dd3f2272168b8483</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2003GL016909$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2003GL016909$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,1427,11493,27901,27902,45550,45551,46384,46443,46808,46867</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=14929481$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Kahn, Brian H.</creatorcontrib><creatorcontrib>Eldering, Annmarie</creatorcontrib><creatorcontrib>Clough, Shepard A.</creatorcontrib><creatorcontrib>Fetzer, Eric J.</creatorcontrib><creatorcontrib>Fishbein, Evan</creatorcontrib><creatorcontrib>Gunson, Michael R.</creatorcontrib><creatorcontrib>Lee, Sung-Yung</creatorcontrib><creatorcontrib>Lester, Peter F.</creatorcontrib><creatorcontrib>Realmuto, Vincent J.</creatorcontrib><title>Near micron-sized cirrus cloud particles in high-resolution infrared spectra: An orographic case study</title><title>Geophysical research letters</title><addtitle>Geophys. Res. Lett</addtitle><description>The high‐resolution spectra of the Atmospheric Infrared Sounder (AIRS) provide a global view of small‐ particle‐dominated cirrus clouds, and they exist over much larger spatial extents than seen in previous aircraft campaigns. As shown by simulations using a plane‐parallel scattering radiative transfer (RT) model and realistic ice particle shapes, the shape of the radiance spectra in the atmospheric windows is uniquely influenced by small ice crystals. Minima in the brightness temperature (BT) spectra between 800 to 850 cm−1 are seen for ice particles smaller than 3 μm in the RT simulations and AIRS spectra. A case study of an orographic cirrus cloud observed on October 2, 2002, over the central Andes of South America is presented with spectral BT differences up to 63K between 998 and 811 cm−1.</description><subject>Cloud physics</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Meteorology</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2003</creationdate><recordtype>article</recordtype><recordid>eNp9kE1P3DAQhq0KJBbaW3-AL-2JgL9ix9wQggVpRUUF4mjNOg7rNpuknkSw_fUYLQJOnGY08zyvNEPId86OOBP2WDAm5wvGtWX2C5lxq1RRMWZ2yIwxm3th9B7ZR_zDMskkn5HmOkCi6-hT3xUY_4ea-pjShNS3_VTTAdIYfRuQxo6u4sOqSAH7dhpj3-VRkyBlBYfgxwQn9LSjfeofEgyr6KkHDBTHqd58JbsNtBi-vdYDcndxfnt2WSx-za_OTheFl6Y0BW_KRlYqcNCiUaBKXaraV0xrvlxKsSylkV4IaxQwDwLKupaNEEZwXS0rVckD8nObO6T-3xRwdOuIPrQtdKGf0AljuVJGZPBwC-bDEVNo3JDiGtLGceZenuk-PjPjP15zAT20-ezOR3x3lBVWVTxzYss9xjZsPs10898Lro02WSq2UsQxPL1JkP66vDWlu7-eO6sFv7-R0l3IZ8IykWU</recordid><startdate>200304</startdate><enddate>200304</enddate><creator>Kahn, Brian H.</creator><creator>Eldering, Annmarie</creator><creator>Clough, Shepard A.</creator><creator>Fetzer, Eric J.</creator><creator>Fishbein, Evan</creator><creator>Gunson, Michael R.</creator><creator>Lee, Sung-Yung</creator><creator>Lester, Peter F.</creator><creator>Realmuto, Vincent J.</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope></search><sort><creationdate>200304</creationdate><title>Near micron-sized cirrus cloud particles in high-resolution infrared spectra: An orographic case study</title><author>Kahn, Brian H. ; Eldering, Annmarie ; Clough, Shepard A. ; Fetzer, Eric J. ; Fishbein, Evan ; Gunson, Michael R. ; Lee, Sung-Yung ; Lester, Peter F. ; Realmuto, Vincent J.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3757-1f5f384e1a62f4a45654dc80661bb32b5373c22974a0ca2a5dd3f2272168b8483</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2003</creationdate><topic>Cloud physics</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Meteorology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kahn, Brian H.</creatorcontrib><creatorcontrib>Eldering, Annmarie</creatorcontrib><creatorcontrib>Clough, Shepard A.</creatorcontrib><creatorcontrib>Fetzer, Eric J.</creatorcontrib><creatorcontrib>Fishbein, Evan</creatorcontrib><creatorcontrib>Gunson, Michael R.</creatorcontrib><creatorcontrib>Lee, Sung-Yung</creatorcontrib><creatorcontrib>Lester, Peter F.</creatorcontrib><creatorcontrib>Realmuto, Vincent J.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kahn, Brian H.</au><au>Eldering, Annmarie</au><au>Clough, Shepard A.</au><au>Fetzer, Eric J.</au><au>Fishbein, Evan</au><au>Gunson, Michael R.</au><au>Lee, Sung-Yung</au><au>Lester, Peter F.</au><au>Realmuto, Vincent J.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Near micron-sized cirrus cloud particles in high-resolution infrared spectra: An orographic case study</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>2003-04</date><risdate>2003</risdate><volume>30</volume><issue>8</issue><spage>24.1</spage><epage>n/a</epage><pages>24.1-n/a</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>The high‐resolution spectra of the Atmospheric Infrared Sounder (AIRS) provide a global view of small‐ particle‐dominated cirrus clouds, and they exist over much larger spatial extents than seen in previous aircraft campaigns. As shown by simulations using a plane‐parallel scattering radiative transfer (RT) model and realistic ice particle shapes, the shape of the radiance spectra in the atmospheric windows is uniquely influenced by small ice crystals. Minima in the brightness temperature (BT) spectra between 800 to 850 cm−1 are seen for ice particles smaller than 3 μm in the RT simulations and AIRS spectra. A case study of an orographic cirrus cloud observed on October 2, 2002, over the central Andes of South America is presented with spectral BT differences up to 63K between 998 and 811 cm−1.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2003GL016909</doi><tpages>4</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0094-8276 |
| ispartof | Geophysical research letters, 2003-04, Vol.30 (8), p.24.1-n/a |
| issn | 0094-8276 1944-8007 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_27914472 |
| source | Wiley-Blackwell AGU Digital Library; Wiley Online Library Journals Frontfile Complete; Wiley Online Library Free Content; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals |
| subjects | Cloud physics Earth, ocean, space Exact sciences and technology External geophysics Meteorology |
| title | Near micron-sized cirrus cloud particles in high-resolution infrared spectra: An orographic case study |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-21T18%3A04%3A34IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Near%20micron-sized%20cirrus%20cloud%20particles%20in%20high-resolution%20infrared%20spectra:%20An%20orographic%20case%20study&rft.jtitle=Geophysical%20research%20letters&rft.au=Kahn,%20Brian%20H.&rft.date=2003-04&rft.volume=30&rft.issue=8&rft.spage=24.1&rft.epage=n/a&rft.pages=24.1-n/a&rft.issn=0094-8276&rft.eissn=1944-8007&rft.coden=GPRLAJ&rft_id=info:doi/10.1029/2003GL016909&rft_dat=%3Cproquest_cross%3E27914472%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=27914472&rft_id=info:pmid/&rfr_iscdi=true |