Climatological Description of Seasonal Variations in Lower-Tropospheric Temperature Inversion Layers over the Indochina Peninsula
In this study operational rawinsonde data are used to investigate climatological features of seasonal variations in static stability in order to understand the behavior of temperature inversion layers, that is, extremely stable layers in the lower troposphere over the Indochina Peninsula region, at...
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| Veröffentlicht in: | Journal of climate 2006-07, Vol.19 (13), p.3307-3319 |
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| creator | Nodzu, Masato I. Ogino, Shin-Ya Tachibana, Yoshihiro Yamanaka, Manabu D. |
| description | In this study operational rawinsonde data are used to investigate climatological features of seasonal variations in static stability in order to understand the behavior of temperature inversion layers, that is, extremely stable layers in the lower troposphere over the Indochina Peninsula region, at the southeastern edge of the Asian continent. Static stability was evaluated from the vertical gradient in potential temperature (Δθ/Δz).
Stable (Δθ/Δz> 10 K km-1) and unstable (Δθ/Δz< 1 K km-1) layers frequently appear over the Indochina Peninsula region during boreal winter. Temporal and vertical variations in stability during the boreal winter can be categorized into three characteristic types, type I: the mean height of stable layers increases from 2 to 5 km from the dry to the rainy season over inland areas of the Indochina Peninsula and southern China; type II: similar to type I, with the additional occurrence of stable layers at a height of ∼1 km, mainly over coastal areas of the Indochina Peninsula; and type III: stable layers at a height of ∼2 km, mainly over the Malay Peninsula. We did not find any significant seasonal change in the vertical distribution of stable layers over the Malay Peninsula. |
| doi_str_mv | 10.1175/jcli3792.1 |
| format | Article |
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Stable (Δθ/Δz> 10 K km-1) and unstable (Δθ/Δz< 1 K km-1) layers frequently appear over the Indochina Peninsula region during boreal winter. Temporal and vertical variations in stability during the boreal winter can be categorized into three characteristic types, type I: the mean height of stable layers increases from 2 to 5 km from the dry to the rainy season over inland areas of the Indochina Peninsula and southern China; type II: similar to type I, with the additional occurrence of stable layers at a height of ∼1 km, mainly over coastal areas of the Indochina Peninsula; and type III: stable layers at a height of ∼2 km, mainly over the Malay Peninsula. We did not find any significant seasonal change in the vertical distribution of stable layers over the Malay Peninsula.</description><identifier>ISSN: 0894-8755</identifier><identifier>EISSN: 1520-0442</identifier><identifier>DOI: 10.1175/jcli3792.1</identifier><language>eng</language><publisher>Boston, MA: American Meteorological Society</publisher><subject>Climate ; Climatic zones ; Climatology ; Coastal zone ; Convection, turbulence, diffusion. Boundary layer structure and dynamics ; Dry seasons ; Earth, ocean, space ; Environmental technology ; Exact sciences and technology ; External geophysics ; Frequency distribution ; Global climate models ; Infrared radiation ; Meteorology ; Rainy season ; Rainy seasons ; Rawinsondes ; Seasonal variations ; Seasons ; Statistical analysis ; Temperature ; Temperature inversions ; Tropical regions ; Troposphere ; Vertical distribution ; Winter</subject><ispartof>Journal of climate, 2006-07, Vol.19 (13), p.3307-3319</ispartof><rights>2006 American Meteorological Society</rights><rights>2006 INIST-CNRS</rights><rights>Copyright American Meteorological Society Jul 1, 2006</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c443t-ece1c939fb82832defc4394b59373d4a74d927975f51d51497083d79d7a2557a3</citedby><cites>FETCH-LOGICAL-c443t-ece1c939fb82832defc4394b59373d4a74d927975f51d51497083d79d7a2557a3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/26259094$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/26259094$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,776,780,799,3668,27901,27902,57992,58225</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=17953921$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Nodzu, Masato I.</creatorcontrib><creatorcontrib>Ogino, Shin-Ya</creatorcontrib><creatorcontrib>Tachibana, Yoshihiro</creatorcontrib><creatorcontrib>Yamanaka, Manabu D.</creatorcontrib><title>Climatological Description of Seasonal Variations in Lower-Tropospheric Temperature Inversion Layers over the Indochina Peninsula</title><title>Journal of climate</title><description>In this study operational rawinsonde data are used to investigate climatological features of seasonal variations in static stability in order to understand the behavior of temperature inversion layers, that is, extremely stable layers in the lower troposphere over the Indochina Peninsula region, at the southeastern edge of the Asian continent. Static stability was evaluated from the vertical gradient in potential temperature (Δθ/Δz).
Stable (Δθ/Δz> 10 K km-1) and unstable (Δθ/Δz< 1 K km-1) layers frequently appear over the Indochina Peninsula region during boreal winter. Temporal and vertical variations in stability during the boreal winter can be categorized into three characteristic types, type I: the mean height of stable layers increases from 2 to 5 km from the dry to the rainy season over inland areas of the Indochina Peninsula and southern China; type II: similar to type I, with the additional occurrence of stable layers at a height of ∼1 km, mainly over coastal areas of the Indochina Peninsula; and type III: stable layers at a height of ∼2 km, mainly over the Malay Peninsula. We did not find any significant seasonal change in the vertical distribution of stable layers over the Malay Peninsula.</description><subject>Climate</subject><subject>Climatic zones</subject><subject>Climatology</subject><subject>Coastal zone</subject><subject>Convection, turbulence, diffusion. Boundary layer structure and dynamics</subject><subject>Dry seasons</subject><subject>Earth, ocean, space</subject><subject>Environmental technology</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Frequency distribution</subject><subject>Global climate models</subject><subject>Infrared radiation</subject><subject>Meteorology</subject><subject>Rainy season</subject><subject>Rainy seasons</subject><subject>Rawinsondes</subject><subject>Seasonal variations</subject><subject>Seasons</subject><subject>Statistical analysis</subject><subject>Temperature</subject><subject>Temperature inversions</subject><subject>Tropical regions</subject><subject>Troposphere</subject><subject>Vertical distribution</subject><subject>Winter</subject><issn>0894-8755</issn><issn>1520-0442</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>BEC</sourceid><sourceid>BENPR</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNpdkc2LFDEQxYMoOK5evAtB0MNCr_nsdI4yq-tIg4Kj1yabrnYy9CRtqlvZo_-5aWZR8FRVr371Dq8Iec7ZFedGvzn6MUhjxRV_QDZcC1YxpcRDsmGNVVVjtH5MniAeGeOiZmxDfm_HcHJzGtP34N1IrwF9DtMcUqRpoF_AYYpF_-ZycKuKNETapl-Qq31OU8LpADl4uofTBNnNSwa6iz8h42rRurvS0VRmOh_WTZ_8IURHP0MMEZfRPSWPBjciPLuvF-Tr-3f77Yeq_XSz275tK6-UnCvwwL2VdrhtRCNFD4NX0qpbbaWRvXJG9VYYa_Sgea-5soY1sje2N05obZy8IK_PvlNOPxbAuTsF9DCOLkJasOOGqboWsoAv_wOPacklBOyEEE3dSNMU6PIM-ZwQMwzdlEuQ-a7jrFtf0X3ctrv1FR0v8Kt7R4cl5CG76AP-uzBWSytW7sWZO-Kc8t-9qIW2zCr5B9GGlC8</recordid><startdate>20060701</startdate><enddate>20060701</enddate><creator>Nodzu, Masato I.</creator><creator>Ogino, Shin-Ya</creator><creator>Tachibana, Yoshihiro</creator><creator>Yamanaka, Manabu D.</creator><general>American Meteorological Society</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7QH</scope><scope>7TG</scope><scope>7UA</scope><scope>7X2</scope><scope>7XB</scope><scope>88F</scope><scope>88I</scope><scope>8AF</scope><scope>8FE</scope><scope>8FG</scope><scope>8FH</scope><scope>8FK</scope><scope>8G5</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M0K</scope><scope>M1Q</scope><scope>M2O</scope><scope>M2P</scope><scope>MBDVC</scope><scope>P5Z</scope><scope>P62</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>S0X</scope></search><sort><creationdate>20060701</creationdate><title>Climatological Description of Seasonal Variations in Lower-Tropospheric Temperature Inversion Layers over the Indochina Peninsula</title><author>Nodzu, Masato I. ; Ogino, Shin-Ya ; Tachibana, Yoshihiro ; Yamanaka, Manabu D.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c443t-ece1c939fb82832defc4394b59373d4a74d927975f51d51497083d79d7a2557a3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>Climate</topic><topic>Climatic zones</topic><topic>Climatology</topic><topic>Coastal zone</topic><topic>Convection, turbulence, diffusion. Boundary layer structure and dynamics</topic><topic>Dry seasons</topic><topic>Earth, ocean, space</topic><topic>Environmental technology</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Frequency distribution</topic><topic>Global climate models</topic><topic>Infrared radiation</topic><topic>Meteorology</topic><topic>Rainy season</topic><topic>Rainy seasons</topic><topic>Rawinsondes</topic><topic>Seasonal variations</topic><topic>Seasons</topic><topic>Statistical analysis</topic><topic>Temperature</topic><topic>Temperature inversions</topic><topic>Tropical regions</topic><topic>Troposphere</topic><topic>Vertical distribution</topic><topic>Winter</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Nodzu, Masato I.</creatorcontrib><creatorcontrib>Ogino, Shin-Ya</creatorcontrib><creatorcontrib>Tachibana, Yoshihiro</creatorcontrib><creatorcontrib>Yamanaka, Manabu D.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Aqualine</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Agricultural Science Collection</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Military Database (Alumni Edition)</collection><collection>Science Database (Alumni Edition)</collection><collection>STEM Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Advanced Technologies & Aerospace Collection</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>eLibrary</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Agricultural Science Database</collection><collection>Military Database</collection><collection>Research Library</collection><collection>Science Database</collection><collection>Research Library (Corporate)</collection><collection>Advanced Technologies & Aerospace Database</collection><collection>ProQuest Advanced Technologies & Aerospace Collection</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>SIRS Editorial</collection><jtitle>Journal of climate</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Nodzu, Masato I.</au><au>Ogino, Shin-Ya</au><au>Tachibana, Yoshihiro</au><au>Yamanaka, Manabu D.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Climatological Description of Seasonal Variations in Lower-Tropospheric Temperature Inversion Layers over the Indochina Peninsula</atitle><jtitle>Journal of climate</jtitle><date>2006-07-01</date><risdate>2006</risdate><volume>19</volume><issue>13</issue><spage>3307</spage><epage>3319</epage><pages>3307-3319</pages><issn>0894-8755</issn><eissn>1520-0442</eissn><abstract>In this study operational rawinsonde data are used to investigate climatological features of seasonal variations in static stability in order to understand the behavior of temperature inversion layers, that is, extremely stable layers in the lower troposphere over the Indochina Peninsula region, at the southeastern edge of the Asian continent. Static stability was evaluated from the vertical gradient in potential temperature (Δθ/Δz).
Stable (Δθ/Δz> 10 K km-1) and unstable (Δθ/Δz< 1 K km-1) layers frequently appear over the Indochina Peninsula region during boreal winter. Temporal and vertical variations in stability during the boreal winter can be categorized into three characteristic types, type I: the mean height of stable layers increases from 2 to 5 km from the dry to the rainy season over inland areas of the Indochina Peninsula and southern China; type II: similar to type I, with the additional occurrence of stable layers at a height of ∼1 km, mainly over coastal areas of the Indochina Peninsula; and type III: stable layers at a height of ∼2 km, mainly over the Malay Peninsula. We did not find any significant seasonal change in the vertical distribution of stable layers over the Malay Peninsula.</abstract><cop>Boston, MA</cop><pub>American Meteorological Society</pub><doi>10.1175/jcli3792.1</doi><tpages>13</tpages><oa>free_for_read</oa></addata></record> |
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| subjects | Climate Climatic zones Climatology Coastal zone Convection, turbulence, diffusion. Boundary layer structure and dynamics Dry seasons Earth, ocean, space Environmental technology Exact sciences and technology External geophysics Frequency distribution Global climate models Infrared radiation Meteorology Rainy season Rainy seasons Rawinsondes Seasonal variations Seasons Statistical analysis Temperature Temperature inversions Tropical regions Troposphere Vertical distribution Winter |
| title | Climatological Description of Seasonal Variations in Lower-Tropospheric Temperature Inversion Layers over the Indochina Peninsula |
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