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text-align: center;\"\u003E\u003Cimg border=\"0\" data-original-height=\"1086\" data-original-width=\"1800\" src=\"https:\/\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEjmTaHzqohI70nqzY2_C6LKgvkO2trmnYlur3qQCsJE7ea02gaSLTfI2p4GnPBU4E84l7sl80e7oBBiiT7j7oH6StMzCLM0N4K5DI6k_533vK0am87aLkkJ6NuT9ExicpGqXWDmzsPFi5lICG-qY7iDsfroXP5p0neR7K-C2izZ7k0bO0Y6okg0BTgnTto\/s16000\/fisika%20atmosfer%20-%20termodinamika%20awan%20dan%20hujan.png\" \/\u003E\n  \u003C\/details\u003E\u003Cbr \/\u003E\n\n\u003Ch3 style=\"text-align: left; color:#1E90FF\"\u003E\u003Ca href=\"https:\/\/www.climate4life.info\/p\/termodinamika-atmosfer.html\"\u003ETermodinamika Atmosfer: Menyelami Fisika Pada Proses di Atmosfer\u003C\/a\u003E\u003C\/h3\u003E\n\n\u003Cstyle\u003E\n.boxdaftar{max-width:200px; position:sticky; float:left; padding-top:10px;  margin-right:15px; border-top:3px solid #219FDE; border-bottom: 2px solid #219FDE; font-size:15px; background-color:rgb(246, 247, 249); line-height:17px; color:} @media screen and (max-width: 767px){.boxdaftar{max-width:430px; margin-right:1px;margin-bottom:35px;padding-top:20px}}\n.boxisi {max-width:430px; position:static; float:left; margin-right:5px; border-bottom:1px solid #219FDE; padding-bottom:10px}\n.accordion {cursor: pointer; margin-left:5px; margin-right:5px; padding: 7px 2px 5px 2px; border-top: 1px solid #219FDE;border-bottom: 0px solid #219FDE; text-align:left; font-size:15px; font-weight:bold}\n.accordion:hover{background-color:rgba(8, 186, 245, 0.7)}\n.panel {display: none; margin-right: 7px; border-top: 0px solid #219FDE;  background-color:;text-align: justify}\n.panel li{min-height:20px; border-bottom: 1px dashed #219FDE; font-size:15px; line-height:17px !important;}\n.panel li a{color:#0033FF} \n.panel li:hover{font-weight:bold}  \n.nolist {list-style-type: none; margin: 0;    padding-left: 18px;}\n\u003C\/style\u003E\n\n\u003Cdiv class=\"boxdaftar\"\u003E\n\u003Ch4 style=\"text-align: center;\"\u003EDaftar Isi\u003C\/h4\u003E\n\n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section1')\"\u003E1. Hukum Tentang Gas\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section1\"\u003E\n\u003Cscript type=\"text\/javascript\"\u003E var numposts = 100; var standardstyling = true; function showrecentposts(json) { for (var i = 0; i \u003C numposts; i++) { var entry = json.feed.entry[i]; var posttitle = entry.title.$t; var posturl; if (i == json.feed.entry.length) break; for (var k = 0; k \u003C entry.link.length; k++) { if (entry.link[k].rel == 'alternate') { posturl = entry.link[k].href; break; }} posttitle = posttitle.link(posturl); if (standardstyling) document.write('\u003Cli\u003E'); document.write(posttitle);} if (standardstyling) document.write('\u003C\/li\u003E'); } \u003C\/script\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap01?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E    \n\u003C\/div\u003E\n  \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section2')\"\u003E2. Persamaan Hidrostatik\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section2\"\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap02?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E    \n\u003C\/div\u003E\n\n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section3')\"\u003E3. Hukum Pertama Termodinamika - Panas dan Kerja Sistem\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section3\"\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap03?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E  \n\u003C\/div\u003E\n  \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section4')\"\u003E4. Proses Adiabatik\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section4\"\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap04?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E \n\u003C\/div\u003E  \n    \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section5')\"\u003E5. Uap Air dalam Udara\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section5\"\u003E  \n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap05?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E \n\u003C\/div\u003E  \n  \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section6')\"\u003E6. Stabilitas Statis\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section6\"\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap06?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E \n\u003C\/div\u003E \n  \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section7')\"\u003E7. Hukum Kedua Termodinamika\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section7\"\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap07?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E \n\u003C\/div\u003E \n  \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section8')\"\u003EReferensi:\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section8\"\u003E\n\u003Cp align=\"left\" style=\"padding-left: 10px;\"\u003EDiterjemahkan dan dikembangkan dari: Atmospheric Thermodynamics, Jeremy A. Gibbs, https:\/\/gibbs.science\/ teaching\/efd\/handouts \/wallace_hobbs_ch3.pdf.\u003C\/p\u003E\n\u003C\/div\u003E\n\n\u003Cscript\u003E\n  function toggleAccordion(sectionId) {\n    var panel = document.getElementById(sectionId);\n    if (panel.style.display === \"block\") {\n      panel.style.display = \"none\";\n    } else {\n      closeAllPanels();\n      panel.style.display = \"block\";\n    }\n  }\n\n  function closeAllPanels() {\n    var panels = document.getElementsByClassName(\"panel\");\n    for (var i = 0; i \u003C panels.length; i++) {\n      panels[i].style.display = \"none\";\n    }\n  }\n\u003C\/script\u003E\n\u003C\/div\u003E\n\n\u003Cdiv class=\"boxisi\"\u003E\n\u003C!------style selesai------\u003E\n\n\n\u003C!------Isi Konten---------\u003E\n  \n\u003Ch3 style=\"text-align: justify;\"\u003EIV. Proses Adiabatik\u003C\/h3\u003E\u003Cdiv style=\"text-align: justify;\"\u003E\u003Ch4\u003EKonsep dasar\u003C\/h4\u003E\u003Cdiv\u003E\u003Cdiv\u003EJika suatu bahan mengalami perubahan dalam keadaan fisiknya (misalnya, tekanan, volume, atau suhu) tanpa adanya penambahan atau pengambilan panas, perubahan tersebut disebut adiabatik.\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003E\u003Ctable align=\"center\" cellpadding=\"0\" cellspacing=\"0\" class=\"tr-caption-container\" style=\"margin-left: auto; margin-right: auto;\"\u003E\u003Ctbody\u003E\u003Ctr\u003E\u003Ctd style=\"text-align: center;\"\u003E\u003Ca href=\"https:\/\/blogger.googleusercontent.com\/img\/a\/AVvXsEgXRb0k9QfPLlWJMtyUzEwopmIjoNaiqmu2y6-k6sd8V6q42jHW2K-7eCltn7ZKcCmP6NFHOeJfjbKdp5g4AlOrEWeGKm-YILNNLdo5okMRqSuBgOSekdpoOwTWM5yFpzWZFhpynqnrNctLLVUr68myZzb1kVaJm4DAizHylx40-oL0zp9AHJseGe4jdiU\" style=\"margin-left: auto; margin-right: auto;\"\u003E\u003Cimg alt=\"\" data-original-height=\"734\" data-original-width=\"840\" height=\"559\" src=\"https:\/\/blogger.googleusercontent.com\/img\/a\/AVvXsEgXRb0k9QfPLlWJMtyUzEwopmIjoNaiqmu2y6-k6sd8V6q42jHW2K-7eCltn7ZKcCmP6NFHOeJfjbKdp5g4AlOrEWeGKm-YILNNLdo5okMRqSuBgOSekdpoOwTWM5yFpzWZFhpynqnrNctLLVUr68myZzb1kVaJm4DAizHylx40-oL0zp9AHJseGe4jdiU=w640-h559\" width=\"640\" \/\u003E\u003C\/a\u003E\u003C\/td\u003E\u003C\/tr\u003E\u003Ctr\u003E\u003Ctd class=\"tr-caption\" style=\"text-align: center;\"\u003EGambar 5 Isoterm dan adiabat pada diagram p–V\u003Cbr \/\u003E\u003Cdiv style=\"text-align: left;\"\u003E\u003Cspan style=\"font-size: small;\"\u003ESumber:\u0026nbsp;https:\/\/www.youphysics.education\/ first-law\/processes \/adiabatic\/\u003C\/span\u003E\u003C\/div\u003E\u003C\/td\u003E\u003C\/tr\u003E\u003C\/tbody\u003E\u003C\/table\u003E\u003Cbr \/\u003E\u003Cbr \/\u003EMisalkan keadaan awal suatu bahan diwakili oleh titik A pada diagram p–V pada Gambar 5 dan ketika bahan mengalami transformasi isotermal (perubahan pada suhu tetap), ia bergerak sepanjang garis TA.\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003EJika bahan yang sama mengalami perubahan volume serupa tetapi dalam kondisi adiabatik, transformasinya akan diwakili oleh kurva seperti AB, yang disebut adiabat.\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003EAlasan mengapa adiabat AB lebih curam daripada isoterm TA pada diagram \\(p–V\\) dapat dilihat sebagai berikut.\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003ESelama kompresi adiabatik, energi internal meningkat karena \\(dq\\) = 0 dan \\(p\\ dα\\) negatif pada \u003Ca href=\"https:\/\/www.climate4life.info\/2023\/10\/konsep-hukum-pertama-termodinamika-atmosfer.html\" target=\"_blank\"\u003Epersamaan (38)\u003C\/a\u003E dan oleh karena itu suhu sistem meningkat.\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003ENamun, untuk kompresi isotermal, suhu tetap konstan. Oleh karena itu, TA \u0026gt; TB dan oleh karena itu pA \u0026gt; pB.\u003C\/div\u003E\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003EUsaha yang dilakukan oleh gas (yang sesuai dengan area yang diarsir dengan warna biru pada diagram PV) dihitung dengan mengintegrasikan persamaan usaha yang dilakukan oleh gas, sebagaimana pada \u003Ca href=\"https:\/\/www.climate4life.info\/2023\/10\/konsep-hukum-pertama-termodinamika-atmosfer.html\" target=\"_blank\"\u003Epersamaan (36)\u003C\/a\u003E\u0026nbsp;yang dapat dituliskan ulang menjadi:\u003C\/div\u003E\u003Cdiv\u003E\\[W_{AB}=\\int_{V_{A}}^{V_{B}} p\\ dV\\]\u003C\/div\u003E\u003C\/div\u003E\u003C\/div\u003E      \n\u003C!--batas konten--\u003E\n\u003Cdiv class=\"separator\" style=\"clear: both;\"\u003E\u003C\/div\u003E"},"link":[{"rel":"replies","type":"application/atom+xml","href":"https:\/\/www.climate4life.info\/feeds\/6587865577692335229\/comments\/default","title":"Post Comments"},{"rel":"replies","type":"text/html","href":"https:\/\/www.climate4life.info\/2023\/10\/proses-adiabatik-termodinamika-atmosfer.html#comment-form","title":"0 Comments"},{"rel":"edit","type":"application/atom+xml","href":"https:\/\/www.blogger.com\/feeds\/8493873891004150846\/posts\/default\/6587865577692335229"},{"rel":"self","type":"application/atom+xml","href":"https:\/\/www.blogger.com\/feeds\/8493873891004150846\/posts\/default\/6587865577692335229"},{"rel":"alternate","type":"text/html","href":"https:\/\/www.climate4life.info\/2023\/10\/proses-adiabatik-termodinamika-atmosfer.html","title":"Konsep Proses Adiabatik"}],"author":[{"name":{"$t":"Climate4life"},"uri":{"$t":"http:\/\/www.blogger.com\/profile\/03747017448251208612"},"email":{"$t":"noreply@blogger.com"},"gd$image":{"rel":"http://schemas.google.com/g/2005#thumbnail","width":"32","height":"32","src":"\/\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEivPePtjvrBk-yk7PLc_-MxpFKrGyM63_X5n1NnKYYGCGsw6YWNSAh3eW6mN7fz8wGOCh9oNWmDri47Uu8BbHhvJLPgviz1B8QvVLZFCWmwpgoO5Wwe0J7a0lRKl3-iEJHdEsnJzL5vA1-s9OhbowA0eiTS8fuJYeMICtcF0gLouAo\/s220\/3.png"}}],"media$thumbnail":{"xmlns$media":"http://search.yahoo.com/mrss/","url":"https:\/\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEjmTaHzqohI70nqzY2_C6LKgvkO2trmnYlur3qQCsJE7ea02gaSLTfI2p4GnPBU4E84l7sl80e7oBBiiT7j7oH6StMzCLM0N4K5DI6k_533vK0am87aLkkJ6NuT9ExicpGqXWDmzsPFi5lICG-qY7iDsfroXP5p0neR7K-C2izZ7k0bO0Y6okg0BTgnTto\/s72-c\/fisika%20atmosfer%20-%20termodinamika%20awan%20dan%20hujan.png","height":"72","width":"72"},"thr$total":{"$t":"0"}},{"id":{"$t":"tag:blogger.com,1999:blog-8493873891004150846.post-8455166135900059744"},"published":{"$t":"2023-10-29T23:00:00.066+07:00"},"updated":{"$t":"2024-01-01T12:38:04.265+07:00"},"category":[{"scheme":"http://www.blogger.com/atom/ns#","term":"02Chap04"},{"scheme":"http://www.blogger.com/atom/ns#","term":"Termodinamika"}],"title":{"type":"text","$t":"Konsep Paket Udara di Atmosfer"},"content":{"type":"html","$t":"\u003C!------style mulai------\u003E\n\u003Cscript src=\"https:\/\/cdnjs.cloudflare.com\/ajax\/libs\/mathjax\/2.7.7\/MathJax.js?config=TeX-MML-AM_CHTML\"\u003E\u003C\/script\u003E\n\n\u003Cdetails\u003E\n\u003Cdiv class=\"separator\" style=\"clear: both; text-align: center;\"\u003E\u003Cimg border=\"0\" data-original-height=\"1086\" data-original-width=\"1800\" src=\"https:\/\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEjmTaHzqohI70nqzY2_C6LKgvkO2trmnYlur3qQCsJE7ea02gaSLTfI2p4GnPBU4E84l7sl80e7oBBiiT7j7oH6StMzCLM0N4K5DI6k_533vK0am87aLkkJ6NuT9ExicpGqXWDmzsPFi5lICG-qY7iDsfroXP5p0neR7K-C2izZ7k0bO0Y6okg0BTgnTto\/s16000\/fisika%20atmosfer%20-%20termodinamika%20awan%20dan%20hujan.png\" \/\u003E\n  \u003C\/details\u003E\u003Cbr \/\u003E\n\n\u003Ch3 style=\"text-align: left; color:#1E90FF\"\u003E\u003Ca href=\"https:\/\/www.climate4life.info\/p\/termodinamika-atmosfer.html\"\u003ETermodinamika Atmosfer: Menyelami Fisika Pada Proses di Atmosfer\u003C\/a\u003E\u003C\/h3\u003E\n\n\u003Cstyle\u003E\n.boxdaftar{max-width:200px; position:sticky; float:left; padding-top:10px;  margin-right:15px; border-top:3px solid #219FDE; border-bottom: 2px solid #219FDE; font-size:15px; background-color:rgb(246, 247, 249); line-height:17px; color:} @media screen and (max-width: 767px){.boxdaftar{max-width:430px; margin-right:1px;margin-bottom:35px;padding-top:20px}}\n.boxisi {max-width:430px; position:static; float:left; margin-right:5px; border-bottom:1px solid #219FDE; padding-bottom:10px}\n.accordion {cursor: pointer; margin-left:5px; margin-right:5px; padding: 7px 2px 5px 2px; border-top: 1px solid #219FDE;border-bottom: 0px solid #219FDE; text-align:left; font-size:15px; font-weight:bold}\n.accordion:hover{background-color:rgba(8, 186, 245, 0.7)}\n.panel {display: none; margin-right: 7px; border-top: 0px solid #219FDE;  background-color:;text-align: justify}\n.panel li{min-height:20px; border-bottom: 1px dashed #219FDE; font-size:15px; line-height:17px !important;}\n.panel li a{color:#0033FF} \n.panel li:hover{font-weight:bold}  \n.nolist {list-style-type: none; margin: 0;    padding-left: 18px;}\n\u003C\/style\u003E\n\n\u003Cdiv class=\"boxdaftar\"\u003E\n\u003Ch4 style=\"text-align: center;\"\u003EDaftar Isi\u003C\/h4\u003E\n\n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section1')\"\u003E1. Hukum Tentang Gas\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section1\"\u003E\n\u003Cscript type=\"text\/javascript\"\u003E var numposts = 100; var standardstyling = true; function showrecentposts(json) { for (var i = 0; i \u003C numposts; i++) { var entry = json.feed.entry[i]; var posttitle = entry.title.$t; var posturl; if (i == json.feed.entry.length) break; for (var k = 0; k \u003C entry.link.length; k++) { if (entry.link[k].rel == 'alternate') { posturl = entry.link[k].href; break; }} posttitle = posttitle.link(posturl); if (standardstyling) document.write('\u003Cli\u003E'); document.write(posttitle);} if (standardstyling) document.write('\u003C\/li\u003E'); } \u003C\/script\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap01?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E    \n\u003C\/div\u003E\n  \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section2')\"\u003E2. Persamaan Hidrostatik\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section2\"\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap02?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E    \n\u003C\/div\u003E\n\n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section3')\"\u003E3. Hukum Pertama Termodinamika - Panas dan Kerja Sistem\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section3\"\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap03?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E  \n\u003C\/div\u003E\n  \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section4')\"\u003E4. Proses Adiabatik\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section4\"\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap04?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E \n\u003C\/div\u003E  \n    \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section5')\"\u003E5. Uap Air dalam Udara\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section5\"\u003E  \n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap05?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E \n\u003C\/div\u003E  \n  \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section6')\"\u003E6. Stabilitas Statis\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section6\"\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap06?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E \n\u003C\/div\u003E \n  \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section7')\"\u003E7. Hukum Kedua Termodinamika\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section7\"\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap07?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E \n\u003C\/div\u003E \n  \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section8')\"\u003EReferensi:\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section8\"\u003E\n\u003Cp align=\"left\" style=\"padding-left: 10px;\"\u003EDiterjemahkan dan dikembangkan dari: Atmospheric Thermodynamics, Jeremy A. Gibbs, https:\/\/gibbs.science\/ teaching\/efd\/handouts \/wallace_hobbs_ch3.pdf.\u003C\/p\u003E\n\u003C\/div\u003E\n\n\u003Cscript\u003E\n  function toggleAccordion(sectionId) {\n    var panel = document.getElementById(sectionId);\n    if (panel.style.display === \"block\") {\n      panel.style.display = \"none\";\n    } else {\n      closeAllPanels();\n      panel.style.display = \"block\";\n    }\n  }\n\n  function closeAllPanels() {\n    var panels = document.getElementsByClassName(\"panel\");\n    for (var i = 0; i \u003C panels.length; i++) {\n      panels[i].style.display = \"none\";\n    }\n  }\n\u003C\/script\u003E\n\u003C\/div\u003E\n\n\u003Cdiv class=\"boxisi\"\u003E\n\u003C!------style selesai------\u003E\n\n\n\u003C!------Isi Konten---------\u003E\n  \n\u003Ch3 style=\"text-align: justify;\"\u003EIV. Proses Adiabatik\u003C\/h3\u003E\u003Cdiv style=\"text-align: justify;\"\u003E\u003Ch4\u003E4.1 Konsep Paket Udara\u003C\/h4\u003E\u003Cdiv\u003E\u003Cdiv\u003EDalam banyak masalah mekanika fluida, pencampuran dianggap sebagai hasil dari gerakan acak molekul individual. Di atmosfer, pencampuran molekuler penting hanya dalam satu sentimeter dari permukaan Bumi dan pada tingkat di atas turbopaus (~105 km).\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003EPada lapisan menengah atmosfer, hampir semua pencampuran secara vertikal dilakukan melalui pertukaran \"paket udara\" makroskala dengan dimensi horizontal mulai dari milimeter hingga skala Bumi itu sendiri.\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003E\u003Ctable cellpadding=\"0\" cellspacing=\"0\" class=\"tr-caption-container\" style=\"margin-left: auto; margin-right: auto; text-align: center;\"\u003E\u003Ctbody\u003E\u003Ctr\u003E\u003Ctd style=\"text-align: center;\"\u003E\u003Ca href=\"https:\/\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEib1ZP-F29t4J_YLNOyR8hg1qL-hNRPDLUCTTCHGgvDlaMnPGESnC6AoMHvuZEUaIwAMq9C4Mp0NXq_U7AFI8bNGo7-xupQDZ42f3MwgW4mXtDQ4sEscMM-wqVNa4YUVUG0E2661WPs-nLY9Lck9uyEE5_p1vHcjralZc0aRiy036QddtKLxx81UW7w3NI\/s1123\/image.png\" style=\"margin-left: auto; margin-right: auto;\"\u003E\u003Cimg border=\"0\" data-original-height=\"1123\" data-original-width=\"1083\" height=\"640\" src=\"https:\/\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEib1ZP-F29t4J_YLNOyR8hg1qL-hNRPDLUCTTCHGgvDlaMnPGESnC6AoMHvuZEUaIwAMq9C4Mp0NXq_U7AFI8bNGo7-xupQDZ42f3MwgW4mXtDQ4sEscMM-wqVNa4YUVUG0E2661WPs-nLY9Lck9uyEE5_p1vHcjralZc0aRiy036QddtKLxx81UW7w3NI\/w618-h640\/image.png\" width=\"618\" \/\u003E\u003C\/a\u003E\u003C\/td\u003E\u003C\/tr\u003E\u003Ctr\u003E\u003Ctd class=\"tr-caption\" style=\"text-align: center;\"\u003EIlustrasi paket udara di atmosfer\u003Cbr \/\u003E\u003Cdiv style=\"text-align: left;\"\u003E\u003Cspan style=\"font-size: small;\"\u003ESumber:\u0026nbsp;https:\/\/www.noaa.gov\/ jetstream\/upperair\/parcel-theory\u003C\/span\u003E\u003C\/div\u003E\u003C\/td\u003E\u003C\/tr\u003E\u003C\/tbody\u003E\u003C\/table\u003E\u003Cdiv class=\"separator\" style=\"clear: both; text-align: center;\"\u003E\u003Cbr \/\u003E\u003C\/div\u003EKonsep paket udara adalah penyederhanaan\u0026nbsp; dari satu kolom gelembung udara yang tidak mempunyai ukuran tertentu yang tetap mempertahankan bentuk dan karakteristik umumnya saat naik atau turun di atmosfer\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003EUntuk mendapatkan wawasan tentang sifat pencampuran vertikal di atmosfer, berguna untuk mempertimbangkan perilaku paket udara dengan dimensi infinitesimal yang diasumsikan:\u003C\/div\u003E\u003Cdiv\u003E\u003Col\u003E\u003Cli\u003EDiinsulasi termal dari lingkungannya sehingga suhunya berubah secara adiabatik saat naik atau turun, selalu tetap pada tekanan yang sama dengan udara lingkungan pada tingkat yang sama, yang diasumsikan berada dalam keseimbangan hidrostatik; dan\u003Cbr \/\u003E\u003Cbr \/\u003E\u003C\/li\u003E\u003Cli\u003EBergerak cukup lambat sehingga energi kinetik makroskopis paket udara merupakan fraksi yang dapat diabaikan dari total energinya.\u003C\/li\u003E\u003C\/ol\u003E\u003Cbr \/\u003EKarena banyaknya pengaruh yang berbeda terhadap kenaikan udara, asumsi di atas tidak selalu benar 100%.\u003Cbr \/\u003E\u003Cbr \/\u003ENamun, teori paket udara ini, masih merupakan cara yang lebih baik untuk memahami faktor-faktor utama dalam bagaimana\u0026nbsp; proses cuaca terjadi atmosfer menghasilkan.\u003C\/div\u003E\u003C\/div\u003E\u003C\/div\u003E\u003C\/div\u003E      \n\u003C!--batas konten--\u003E\n\u003Cdiv class=\"separator\" style=\"clear: both;\"\u003E\u003C\/div\u003E"},"link":[{"rel":"replies","type":"application/atom+xml","href":"https:\/\/www.climate4life.info\/feeds\/8455166135900059744\/comments\/default","title":"Post Comments"},{"rel":"replies","type":"text/html","href":"https:\/\/www.climate4life.info\/2023\/10\/konsep-paket-udara-termodinamika-atmosfer.html#comment-form","title":"0 Comments"},{"rel":"edit","type":"application/atom+xml","href":"https:\/\/www.blogger.com\/feeds\/8493873891004150846\/posts\/default\/8455166135900059744"},{"rel":"self","type":"application/atom+xml","href":"https:\/\/www.blogger.com\/feeds\/8493873891004150846\/posts\/default\/8455166135900059744"},{"rel":"alternate","type":"text/html","href":"https:\/\/www.climate4life.info\/2023\/10\/konsep-paket-udara-termodinamika-atmosfer.html","title":"Konsep Paket Udara di Atmosfer"}],"author":[{"name":{"$t":"Climate4life"},"uri":{"$t":"http:\/\/www.blogger.com\/profile\/03747017448251208612"},"email":{"$t":"noreply@blogger.com"},"gd$image":{"rel":"http://schemas.google.com/g/2005#thumbnail","width":"32","height":"32","src":"\/\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEivPePtjvrBk-yk7PLc_-MxpFKrGyM63_X5n1NnKYYGCGsw6YWNSAh3eW6mN7fz8wGOCh9oNWmDri47Uu8BbHhvJLPgviz1B8QvVLZFCWmwpgoO5Wwe0J7a0lRKl3-iEJHdEsnJzL5vA1-s9OhbowA0eiTS8fuJYeMICtcF0gLouAo\/s220\/3.png"}}],"media$thumbnail":{"xmlns$media":"http://search.yahoo.com/mrss/","url":"https:\/\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEjmTaHzqohI70nqzY2_C6LKgvkO2trmnYlur3qQCsJE7ea02gaSLTfI2p4GnPBU4E84l7sl80e7oBBiiT7j7oH6StMzCLM0N4K5DI6k_533vK0am87aLkkJ6NuT9ExicpGqXWDmzsPFi5lICG-qY7iDsfroXP5p0neR7K-C2izZ7k0bO0Y6okg0BTgnTto\/s72-c\/fisika%20atmosfer%20-%20termodinamika%20awan%20dan%20hujan.png","height":"72","width":"72"},"thr$total":{"$t":"0"}},{"id":{"$t":"tag:blogger.com,1999:blog-8493873891004150846.post-2628822304641448015"},"published":{"$t":"2023-10-29T22:00:00.135+07:00"},"updated":{"$t":"2024-01-01T12:38:19.603+07:00"},"category":[{"scheme":"http://www.blogger.com/atom/ns#","term":"02Chap04"},{"scheme":"http://www.blogger.com/atom/ns#","term":"Termodinamika"}],"title":{"type":"text","$t":"Laju Penurunan Adiabatik Kering"},"content":{"type":"html","$t":"\u003C!------style mulai------\u003E\n\u003Cscript src=\"https:\/\/cdnjs.cloudflare.com\/ajax\/libs\/mathjax\/2.7.7\/MathJax.js?config=TeX-MML-AM_CHTML\"\u003E\u003C\/script\u003E\n\n\u003Cdetails\u003E\n\u003Cdiv class=\"separator\" style=\"clear: both; text-align: center;\"\u003E\u003Cimg border=\"0\" data-original-height=\"1086\" data-original-width=\"1800\" src=\"https:\/\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEjmTaHzqohI70nqzY2_C6LKgvkO2trmnYlur3qQCsJE7ea02gaSLTfI2p4GnPBU4E84l7sl80e7oBBiiT7j7oH6StMzCLM0N4K5DI6k_533vK0am87aLkkJ6NuT9ExicpGqXWDmzsPFi5lICG-qY7iDsfroXP5p0neR7K-C2izZ7k0bO0Y6okg0BTgnTto\/s16000\/fisika%20atmosfer%20-%20termodinamika%20awan%20dan%20hujan.png\" \/\u003E\n  \u003C\/details\u003E\u003Cbr \/\u003E\n\n\u003Ch3 style=\"text-align: left; color:#1E90FF\"\u003E\u003Ca href=\"https:\/\/www.climate4life.info\/p\/termodinamika-atmosfer.html\"\u003ETermodinamika Atmosfer: Menyelami Fisika Pada Proses di Atmosfer\u003C\/a\u003E\u003C\/h3\u003E\n\n\u003Cstyle\u003E\n.boxdaftar{max-width:200px; position:sticky; float:left; padding-top:10px;  margin-right:15px; border-top:3px solid #219FDE; border-bottom: 2px solid #219FDE; font-size:15px; background-color:rgb(246, 247, 249); line-height:17px; color:} @media screen and (max-width: 767px){.boxdaftar{max-width:430px; 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Proses Adiabatik\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section4\"\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap04?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E \n\u003C\/div\u003E  \n    \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section5')\"\u003E5. Uap Air dalam Udara\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section5\"\u003E  \n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap05?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E \n\u003C\/div\u003E  \n  \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section6')\"\u003E6. 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Hukum Kedua Termodinamika\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section7\"\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap07?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E \n\u003C\/div\u003E \n  \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section8')\"\u003EReferensi:\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section8\"\u003E\n\u003Cp align=\"left\" style=\"padding-left: 10px;\"\u003EDiterjemahkan dan dikembangkan dari: Atmospheric Thermodynamics, Jeremy A. Gibbs, https:\/\/gibbs.science\/ teaching\/efd\/handouts \/wallace_hobbs_ch3.pdf.\u003C\/p\u003E\n\u003C\/div\u003E\n\n\u003Cscript\u003E\n  function toggleAccordion(sectionId) {\n    var panel = document.getElementById(sectionId);\n    if (panel.style.display === \"block\") {\n      panel.style.display = \"none\";\n    } else {\n      closeAllPanels();\n      panel.style.display = \"block\";\n    }\n  }\n\n  function closeAllPanels() {\n    var panels = document.getElementsByClassName(\"panel\");\n    for (var i = 0; i \u003C panels.length; i++) {\n      panels[i].style.display = \"none\";\n    }\n  }\n\u003C\/script\u003E\n\u003C\/div\u003E\n\n\u003Cdiv class=\"boxisi\"\u003E\n\u003C!------style selesai------\u003E\n\n\n\u003C!------Isi Konten---------\u003E\n  \n\u003Ch3 style=\"text-align: justify;\"\u003EIV. Proses Adiabatik\u003C\/h3\u003E\u003Cdiv style=\"text-align: justify;\"\u003E\u003Ch4\u003E4.2 Laju Penurunan Adiabatik Kering\u003C\/h4\u003E\u003Cdiv\u003E\u003Cdiv\u003ESekarang kita akan turunkan persamaan untuk laju perubahan suhu terhadap ketinggian dari sejumlah udara kering yang bergerak di atmosfer Bumi selalu memenuhi kondisi yang tercantum pada akhir \u003Ca href=\"https:\/\/www.climate4life.info\/2023\/10\/proses-adiabatik-termodinamika-atmosfer.html\" target=\"_blank\"\u003EBagian 4.1\u003C\/a\u003E.\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003EKarena paket udara hanya mengalami transformasi adiabatik (\\(dq\\) = 0) dan atmosfer berada dalam keseimbangan hidrostatik, untuk satu massa udara dalam paket, berdasarkan\u0026nbsp;\u003Ca href=\"https:\/\/www.climate4life.info\/2023\/10\/entalpi-termodinamika-atmosfer.html\" target=\"_blank\"\u003Epersamaan (51)\u003C\/a\u003E,\u003C\/div\u003E\n  \n\\begin{align*}\nd(c_{p}\\ T + \\phi) \u0026amp;=0\\\\\ndT\\ c_{p} +d \\phi \u0026amp;=0 \\tag {52}\n\\end{align*}\n  \n\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003EDengan menggunakan \\(d\\phi = g\\ dz\\) dari \u003Ca href=\"https:\/\/www.climate4life.info\/2023\/10\/ketinggian-geopotensial-termodinamika-atmosfer.html\" target=\"_blank\"\u003Epersamaan (3.20)\u003C\/a\u003E, maka:\u003C\/div\u003E\n  \n\\begin{align*}\ndT\\ c_{p} + g\\ dz  \u0026amp;=0\\\\\n-dT\\ c_{p} \u0026amp;= g\\ dz \\\\\n-\\left (\\frac{dT}{dz} \\right ) \u0026amp;= \\frac{g}{c_{p}} \\\\\n-\\left (\\frac{dT}{dz} \\right )_{dry\\ parcel}\u0026amp;= \\frac{g}{c_{p}}\\equiv  \\Gamma_{d}\n\\end{align*}\n\n\u003Cdiv style=\"text-align: right;\"\u003E(53)\n\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003Edi mana \\(\\Gamma_d\\) disebut sebagai \u003Cb\u003Elaju penurunan adiabatik kering\u003C\/b\u003E.\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003EKarena paket udara mengembang saat naik di atmosfer, suhunya akan turun seiring dengan ketinggian sehingga \\(\\Gamma_d\\) yang didefinisikan oleh persamaan (53) bernilai positif.\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003EDengan memasukkan \\(g\\)= 9,8 m s\\(^{-2}\\) dan \\(c_p\\)= 1005 J ⁰C\\(^{-1}\\) kg\\(^{-1}\\) ke dalam persamaan (53), maka:\u003C\/div\u003E\n\n\\begin{align*}\n\\require{cancel}\n\\Gamma_{d} \u0026amp;=\\frac{9.8\\ m\\ s^{-2}}{1005\\ Jkg^{-1}\\ ^{0}C^{-1}}\\\\\n\\Gamma_{d} \u0026amp;=\\frac{9.8\\ \\bcancel m \\bcancel s^{-2}\\ ^{0}C}{1005\\ \\bcancel {kg} m^ {\\bcancel 2} \\bcancel s^{-2} \\bcancel {kg} ^{-1}\\ }\\\\\n\\Gamma_{d} \u0026amp;=\\frac{9.8\\ ^{0}C}{1005\\ m}\\\\\n\\Gamma_{d} \u0026amp;=\\frac{0.98\\ ^{0}C}{100.5\\ m}\\\\\\\\\n\\Gamma_{d} \u0026amp;\\equiv \\frac{1\\ ^{0}C}{100\\ m}\n\\end{align*}\n  \n\n\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003EHasil \\(\\Gamma_d\\) 1 ⁰C\/100 m atau 9,8 K km\\(^{-1}\\), merupakan nilai numerik dari laju penurunan adiabatik kering.\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003EPerlu ditekankan lagi bahwa \\(\\Gamma_d\\) adalah laju perubahan suhu mengikuti paket udara kering yang sedang diangkat atau diturunkan secara adiabatik di atmosfer.\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003ELaju penurunan aktual suhu dalam kolom udara, yang akan kita tunjukkan dengan \\(\\Gamma\\) = dT\/dz, seperti yang diukur, misalnya, oleh radiosonde, rata-rata 6–7 K km\\(^{-1}\\) di troposfer, tetapi bervariasi pada berbagai tempat berbeda.\u003C\/div\u003E\u003C\/div\u003E\u003C\/div\u003E\u003C\/div\u003E      \n\u003C!--batas konten--\u003E\n\u003Cdiv class=\"separator\" style=\"clear: both;\"\u003E\u003C\/div\u003E"},"link":[{"rel":"replies","type":"application/atom+xml","href":"https:\/\/www.climate4life.info\/feeds\/2628822304641448015\/comments\/default","title":"Post 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Kering"}],"author":[{"name":{"$t":"Climate4life"},"uri":{"$t":"http:\/\/www.blogger.com\/profile\/03747017448251208612"},"email":{"$t":"noreply@blogger.com"},"gd$image":{"rel":"http://schemas.google.com/g/2005#thumbnail","width":"32","height":"32","src":"\/\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEivPePtjvrBk-yk7PLc_-MxpFKrGyM63_X5n1NnKYYGCGsw6YWNSAh3eW6mN7fz8wGOCh9oNWmDri47Uu8BbHhvJLPgviz1B8QvVLZFCWmwpgoO5Wwe0J7a0lRKl3-iEJHdEsnJzL5vA1-s9OhbowA0eiTS8fuJYeMICtcF0gLouAo\/s220\/3.png"}}],"media$thumbnail":{"xmlns$media":"http://search.yahoo.com/mrss/","url":"https:\/\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEjmTaHzqohI70nqzY2_C6LKgvkO2trmnYlur3qQCsJE7ea02gaSLTfI2p4GnPBU4E84l7sl80e7oBBiiT7j7oH6StMzCLM0N4K5DI6k_533vK0am87aLkkJ6NuT9ExicpGqXWDmzsPFi5lICG-qY7iDsfroXP5p0neR7K-C2izZ7k0bO0Y6okg0BTgnTto\/s72-c\/fisika%20atmosfer%20-%20termodinamika%20awan%20dan%20hujan.png","height":"72","width":"72"},"thr$total":{"$t":"0"}},{"id":{"$t":"tag:blogger.com,1999:blog-8493873891004150846.post-4710261954554724722"},"published":{"$t":"2023-10-28T23:00:00.157+07:00"},"updated":{"$t":"2024-01-01T12:38:28.073+07:00"},"category":[{"scheme":"http://www.blogger.com/atom/ns#","term":"02Chap04"},{"scheme":"http://www.blogger.com/atom/ns#","term":"Termodinamika"}],"title":{"type":"text","$t":"Temperatur Potensial - Persamaan Poisson"},"content":{"type":"html","$t":"\u003C!------style mulai------\u003E\n\u003Cscript src=\"https:\/\/cdnjs.cloudflare.com\/ajax\/libs\/mathjax\/2.7.7\/MathJax.js?config=TeX-MML-AM_CHTML\"\u003E\u003C\/script\u003E\n\n\u003Cdetails\u003E\n\u003Cdiv class=\"separator\" style=\"clear: both; text-align: center;\"\u003E\u003Cimg border=\"0\" data-original-height=\"1086\" data-original-width=\"1800\" src=\"https:\/\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEjmTaHzqohI70nqzY2_C6LKgvkO2trmnYlur3qQCsJE7ea02gaSLTfI2p4GnPBU4E84l7sl80e7oBBiiT7j7oH6StMzCLM0N4K5DI6k_533vK0am87aLkkJ6NuT9ExicpGqXWDmzsPFi5lICG-qY7iDsfroXP5p0neR7K-C2izZ7k0bO0Y6okg0BTgnTto\/s16000\/fisika%20atmosfer%20-%20termodinamika%20awan%20dan%20hujan.png\" \/\u003E\n  \u003C\/details\u003E\u003Cbr \/\u003E\n\n\u003Ch3 style=\"text-align: left; color:#1E90FF\"\u003E\u003Ca href=\"https:\/\/www.climate4life.info\/p\/termodinamika-atmosfer.html\"\u003ETermodinamika Atmosfer: Menyelami Fisika 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Persamaan Hidrostatik\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section2\"\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap02?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E    \n\u003C\/div\u003E\n\n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section3')\"\u003E3. Hukum Pertama Termodinamika - Panas dan Kerja Sistem\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section3\"\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap03?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E  \n\u003C\/div\u003E\n  \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section4')\"\u003E4. Proses Adiabatik\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section4\"\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap04?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E \n\u003C\/div\u003E  \n    \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section5')\"\u003E5. Uap Air dalam Udara\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section5\"\u003E  \n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap05?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E \n\u003C\/div\u003E  \n  \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section6')\"\u003E6. Stabilitas Statis\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section6\"\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap06?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E \n\u003C\/div\u003E \n  \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section7')\"\u003E7. Hukum Kedua Termodinamika\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section7\"\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap07?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E \n\u003C\/div\u003E \n  \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section8')\"\u003EReferensi:\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section8\"\u003E\n\u003Cp align=\"left\" style=\"padding-left: 10px;\"\u003EDiterjemahkan dan dikembangkan dari: Atmospheric Thermodynamics, Jeremy A. Gibbs, https:\/\/gibbs.science\/ teaching\/efd\/handouts \/wallace_hobbs_ch3.pdf.\u003C\/p\u003E\n\u003C\/div\u003E\n\n\u003Cscript\u003E\n  function toggleAccordion(sectionId) {\n    var panel = document.getElementById(sectionId);\n    if (panel.style.display === \"block\") {\n      panel.style.display = \"none\";\n    } else {\n      closeAllPanels();\n      panel.style.display = \"block\";\n    }\n  }\n\n  function closeAllPanels() {\n    var panels = document.getElementsByClassName(\"panel\");\n    for (var i = 0; i \u003C panels.length; i++) {\n      panels[i].style.display = \"none\";\n    }\n  }\n\u003C\/script\u003E\n\u003C\/div\u003E\n\n\u003Cdiv class=\"boxisi\"\u003E\n\u003C!------style selesai------\u003E\n\n\n\u003C!------Isi Konten---------\u003E\n  \n\u003Ch3 style=\"text-align: justify;\"\u003EIV. Proses Adiabatik\u003C\/h3\u003E\u003Cdiv style=\"text-align: justify;\"\u003E\u003Ch4\u003E4.3 Temperatur Potensial\u003C\/h4\u003E\u003Cdiv\u003E\u003Cdiv\u003ETemperatur potensial θ dari suatu paket udara didefinisikan sebagai suhu yang dimiliki paket udara tersebut jika memuai atau dikompresi secara adiabatik dari tekanan dan suhu eksistingnya menjadi tekanan standar \\( p_{0} \\) (biasanya 1000 hPa).\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003EKita dapat menuliskan ekspresi untuk temperatur potensial dari suatu paket udara dalam hal tekanannya \\( p \\), suhunya \\( T \\), dan tekanan standar \\( p_{0} \\) sebagai berikut. Untuk transformasi adiabatik (\\(dq\\) = 0), pada \u003Ca href=\"https:\/\/www.climate4life.info\/2023\/10\/panas-spesifik-termodinamika-atmosfer.html\" target=\"_blank\"\u003Epersamaan (46)\u003C\/a\u003E menjadi:\u003C\/div\u003E\n\n\u003Cdiv\u003E\\[cp\\ dT - \\alpha\\ dp = 0\\]\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\n\u003Cdiv\u003EKita substitusi \\( \\alpha \\) dari \u003Ca href=\"https:\/\/www.climate4life.info\/2023\/10\/konsep-hukum-pertama-termodinamika-atmosfer.html\" target=\"_blank\"\u003Epersamaan (33)\u003C\/a\u003E ke dalam persamaan di atas menghasilkan:\u003C\/div\u003E\n\n\u003Cdiv\u003E\\[\\frac{c_{p}}{R}\\frac{dT}{T}-\\frac{dp}{P}=0\\]\u003C\/div\u003E\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003E\n\u003Cdiv\u003EPersamaan di atas diintegralkan dari \\( p_{0} \\)\u0026nbsp; ke \\( p \\), dimana, \\( T = \\theta \\), maka kita dapatkan:\u003C\/div\u003E\n  \n\u003Cdiv\u003E\\[\\frac{c_{p}}{R} \\int_{\\theta }^{}\\frac{dT}{T} = \\int_{p_{0}}^{p}\\frac{dp}{P}\\]\u003C\/div\u003E\n  \n\u003Cdiv\u003Eatau,\u003C\/div\u003E\n\u003Cdiv\u003E\\[\\frac{c_{p}}{R} \\ln\\frac{T}{\\theta } = \\ln \\frac{p}{p_{0}}\\]\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\n  \n\u003Cdiv\u003EMengambil antilog pada kedua ruas,\u003C\/div\u003E\n\u003Cdiv\u003E\\[\\left(\\frac{T}{\\theta }\\right)^{c_{p}\/R}=\\frac{p}{p_{0}}\\]\u003C\/div\u003E\n  \n\u003Cdiv\u003Eatau,\u003C\/div\u003E\n\n\u003Cdiv\u003E\\[\\theta =T\\left ( \\frac{p_{0}}{p} \\right )^{R\/c_{p}} \\tag {54}\\]\u003Cbr \/\u003E\u003Cbr \/\u003EPersamaan (54) disebut sebagai persamaan Poisson.\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\n  \u003C\/div\u003E\n\n  \u003Cdetails\u003E\u003Csummary\u003EPoisson\u003C\/summary\u003E\n  Simeon Denis Poisson (1781–1840); adalah seorang matematikawan Prancis. Ia mempelajari kedokteran tetapi beralih ke matematika terapan dan menjadi profesor mekanika pertama di Sorbonne, Paris.\u003C\/details\u003E\n  \n\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\n\u003Cdiv\u003EDiasumsikan bahwa\u003C\/div\u003E\u003Cdiv\u003E\u003Cul\u003E\u003Cli\u003E\u0026nbsp;\\( R \\) ≃ \\( R_{d} \\) adalah sekitar 287 \\(JK^{-1}kg^{-1}\\) dan\u003C\/li\u003E\u003Cli\u003E\u0026nbsp;\\( c_{p} ≃\u0026nbsp;c_{pd}\\) = 1004 \\( JK^{-1}kg^{-1} \\); oleh karena itu,\u0026nbsp;\u003C\/li\u003E\u003Cli\u003E\\( R\/c_{p} \\)\u0026nbsp; setara dengan 0,286.\u003C\/li\u003E\u003C\/ul\u003E\u003C\/div\u003E\u003C\/div\u003E\u003Cdiv\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003EParameter yang tetap konstan selama transformasi tertentu disebut konservatif. Temperatur potensial adalah suatu besaran konservatif untuk suatu paket udara yang bergerak di atmosfer dalam kondisi adiabatik (lihat Latihan 3.36).\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003ETemperatur potensial adalah parameter yang sangat berguna dalam termodinamika atmosfer, karena proses atmosfer seringkali mendekati adiabatik, dan oleh karena itu \\( \\theta \\) tetap pada dasarnya konstan, seperti halnya densitas dalam fluida yang tidak dapat dipampatkan.\u003C\/div\u003E\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003C\/div\u003E\u003C\/div\u003E \n\n\n\u003C!--batas konten--\u003E\n\u003Cdiv class=\"separator\" style=\"clear: both;\"\u003E\u003C\/div\u003E"},"link":[{"rel":"replies","type":"application/atom+xml","href":"https:\/\/www.climate4life.info\/feeds\/4710261954554724722\/comments\/default","title":"Post Comments"},{"rel":"replies","type":"text/html","href":"https:\/\/www.climate4life.info\/2023\/10\/temperatur-potensial-termodinamika-atmosfer.html#comment-form","title":"0 Comments"},{"rel":"edit","type":"application/atom+xml","href":"https:\/\/www.blogger.com\/feeds\/8493873891004150846\/posts\/default\/4710261954554724722"},{"rel":"self","type":"application/atom+xml","href":"https:\/\/www.blogger.com\/feeds\/8493873891004150846\/posts\/default\/4710261954554724722"},{"rel":"alternate","type":"text/html","href":"https:\/\/www.climate4life.info\/2023\/10\/temperatur-potensial-termodinamika-atmosfer.html","title":"Temperatur Potensial - Persamaan Poisson"}],"author":[{"name":{"$t":"Climate4life"},"uri":{"$t":"http:\/\/www.blogger.com\/profile\/03747017448251208612"},"email":{"$t":"noreply@blogger.com"},"gd$image":{"rel":"http://schemas.google.com/g/2005#thumbnail","width":"32","height":"32","src":"\/\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEivPePtjvrBk-yk7PLc_-MxpFKrGyM63_X5n1NnKYYGCGsw6YWNSAh3eW6mN7fz8wGOCh9oNWmDri47Uu8BbHhvJLPgviz1B8QvVLZFCWmwpgoO5Wwe0J7a0lRKl3-iEJHdEsnJzL5vA1-s9OhbowA0eiTS8fuJYeMICtcF0gLouAo\/s220\/3.png"}}],"media$thumbnail":{"xmlns$media":"http://search.yahoo.com/mrss/","url":"https:\/\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEjmTaHzqohI70nqzY2_C6LKgvkO2trmnYlur3qQCsJE7ea02gaSLTfI2p4GnPBU4E84l7sl80e7oBBiiT7j7oH6StMzCLM0N4K5DI6k_533vK0am87aLkkJ6NuT9ExicpGqXWDmzsPFi5lICG-qY7iDsfroXP5p0neR7K-C2izZ7k0bO0Y6okg0BTgnTto\/s72-c\/fisika%20atmosfer%20-%20termodinamika%20awan%20dan%20hujan.png","height":"72","width":"72"},"thr$total":{"$t":"0"}},{"id":{"$t":"tag:blogger.com,1999:blog-8493873891004150846.post-6387086034618372383"},"published":{"$t":"2023-10-28T22:30:00.152+07:00"},"updated":{"$t":"2024-01-01T12:38:35.105+07:00"},"category":[{"scheme":"http://www.blogger.com/atom/ns#","term":"02Chap04"},{"scheme":"http://www.blogger.com/atom/ns#","term":"Termodinamika"}],"title":{"type":"text","$t":"Diagram Termodinamika Skew T-ln P"},"content":{"type":"html","$t":"\u003C!------style mulai------\u003E\n\u003Cscript src=\"https:\/\/cdnjs.cloudflare.com\/ajax\/libs\/mathjax\/2.7.7\/MathJax.js?config=TeX-MML-AM_CHTML\"\u003E\u003C\/script\u003E\n\n\u003Cdetails\u003E\n\u003Cdiv class=\"separator\" style=\"clear: both; text-align: center;\"\u003E\u003Cimg border=\"0\" data-original-height=\"1086\" data-original-width=\"1800\" src=\"https:\/\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEjmTaHzqohI70nqzY2_C6LKgvkO2trmnYlur3qQCsJE7ea02gaSLTfI2p4GnPBU4E84l7sl80e7oBBiiT7j7oH6StMzCLM0N4K5DI6k_533vK0am87aLkkJ6NuT9ExicpGqXWDmzsPFi5lICG-qY7iDsfroXP5p0neR7K-C2izZ7k0bO0Y6okg0BTgnTto\/s16000\/fisika%20atmosfer%20-%20termodinamika%20awan%20dan%20hujan.png\" \/\u003E\n  \u003C\/details\u003E\u003Cbr \/\u003E\n\n\u003Ch3 style=\"text-align: left; color:#1E90FF\"\u003E\u003Ca href=\"https:\/\/www.climate4life.info\/p\/termodinamika-atmosfer.html\"\u003ETermodinamika Atmosfer: Menyelami Fisika Pada Proses di Atmosfer\u003C\/a\u003E\u003C\/h3\u003E\n\n\u003Cstyle\u003E\n.boxdaftar{max-width:200px; position:sticky; float:left; padding-top:10px;  margin-right:15px; border-top:3px solid #219FDE; border-bottom: 2px solid #219FDE; font-size:15px; background-color:rgb(246, 247, 249); line-height:17px; color:} @media screen and (max-width: 767px){.boxdaftar{max-width:430px; 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Proses Adiabatik\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section4\"\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap04?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E \n\u003C\/div\u003E  \n    \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section5')\"\u003E5. Uap Air dalam Udara\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section5\"\u003E  \n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap05?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E \n\u003C\/div\u003E  \n  \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section6')\"\u003E6. Stabilitas Statis\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section6\"\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap06?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E \n\u003C\/div\u003E \n  \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section7')\"\u003E7. Hukum Kedua Termodinamika\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section7\"\u003E\n\u003Cdiv class=\"nolist\"\u003E \u003Cscript src=\"https:\/\/climate4life.info\/feeds\/posts\/default\/-\/02Chap07?orderby=published\u0026amp;alt=json-in-script\u0026amp;callback=showrecentposts\u0026amp;max-results=999\"\u003E\u003C\/script\u003E\u003C\/div\u003E \n\u003C\/div\u003E \n  \n\u003Cdiv class=\"accordion\" onclick=\"toggleAccordion('section8')\"\u003EReferensi:\u003C\/div\u003E\n\u003Cdiv class=\"panel\" id=\"section8\"\u003E\n\u003Cp align=\"left\" style=\"padding-left: 10px;\"\u003EDiterjemahkan dan dikembangkan dari: Atmospheric Thermodynamics, Jeremy A. Gibbs, https:\/\/gibbs.science\/ teaching\/efd\/handouts \/wallace_hobbs_ch3.pdf.\u003C\/p\u003E\n\u003C\/div\u003E\n\n\u003Cscript\u003E\n  function toggleAccordion(sectionId) {\n    var panel = document.getElementById(sectionId);\n    if (panel.style.display === \"block\") {\n      panel.style.display = \"none\";\n    } else {\n      closeAllPanels();\n      panel.style.display = \"block\";\n    }\n  }\n\n  function closeAllPanels() {\n    var panels = document.getElementsByClassName(\"panel\");\n    for (var i = 0; i \u003C panels.length; i++) {\n      panels[i].style.display = \"none\";\n    }\n  }\n\u003C\/script\u003E\n\u003C\/div\u003E\n\n\u003Cdiv class=\"boxisi\"\u003E\n\u003C!------style selesai------\u003E\n\n\n\u003C!------Isi Konten---------\u003E\n  \n\u003Ch3 style=\"text-align: justify;\"\u003EIV. Proses Adiabatik\u003C\/h3\u003E\u003Cdiv\u003E\u003Ch4\u003E4.4 Diagram Termodinamika Skew T -ln P\u003C\/h4\u003E\u003Cdiv\u003E\u003Cdiv style=\"text-align: justify;\"\u003E\u003Ca href=\"https:\/\/www.climate4life.info\/2023\/10\/temperatur-potensial-termodinamika-atmosfer.html\" target=\"_blank\"\u003EPersamaan Poisson\u003C\/a\u003E dapat dipecahkan dengan mudah dalam bentuk grafis.\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003E\u003Cdiv style=\"text-align: justify;\"\u003EJika tekanan digambarkan pada ordinat pada skala yang distorsi, di mana jarak dari titik asal sebanding dengan \\( R\/c_{p} \\) atau \\( p = 0.286 \\) digunakan, tanpa memperhatikan apakah udara kering atau lembab, dan suhu (dalam K) digambarkan pada absis, maka persamaan (54) menjadi:\u003C\/div\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003C\/div\u003E\u003Cdiv style=\"text-align: center;\"\u003E\\(p^{^{0.286}}=\\left (\u0026nbsp; \\frac{(p_{0})^{^{0.286}}}{\\theta }\\right )T \\)\u003C\/div\u003E\u003Cdiv style=\"text-align: right;\"\u003E(55)\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003E\u003Cdiv style=\"text-align: justify;\"\u003EUntuk nilai tetap θ, persamaan (55) memiliki bentuk \\(y\\) ∝ \\(x\\), di mana y = \\(p^{0.286}\\), \\(x\\) = \\(T\\), dan konstanta proporsionalitasnya adalah \\( (p_{0})^{0.286} \/\\theta \\). Setiap nilai tetap θ mewakili adiabat kering, yang didefinisikan oleh garis lurus dengan kemiringan tertentu yang melewati titik \\(p\\) = 0, \\(T\\) = 0.\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003EJika skala tekanan diinversi sehingga \\(p\\) meningkat ke bawah, hubungan tersebut mengambil bentuk yang ditunjukkan dalam Gambar 6, yang merupakan dasar bagi diagram pseudoadiabatik yang banyak digunakan untuk perhitungan meteorologi.\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003E\u003Ctable cellpadding=\"0\" cellspacing=\"0\" class=\"tr-caption-container\" style=\"margin-left: auto; margin-right: auto; text-align: justify;\"\u003E\u003Ctbody\u003E\u003Ctr\u003E\u003Ctd style=\"text-align: center;\"\u003E\u003Ca href=\"https:\/\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEgiWy-cPAWyJuMZQHTEHw7Q4obOazvCUCMnWJdFco39cOai_W1VndALGRSQ44mkQGhuwZznaRlBf71H1tvNKgFVn5fl4VtuSoVQURDYNpnNH2upESXnMXa02Gy3VAZhTherpljiwknz9-tR1d-2oqUJzejQJQ7vqXS4SlJ3w3MxEXoDGBbstisQ85zQwu8\/s798\/image.png\" style=\"margin-left: auto; margin-right: auto;\"\u003E\u003Cimg border=\"0\" data-original-height=\"798\" data-original-width=\"764\" height=\"640\" src=\"https:\/\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEgiWy-cPAWyJuMZQHTEHw7Q4obOazvCUCMnWJdFco39cOai_W1VndALGRSQ44mkQGhuwZznaRlBf71H1tvNKgFVn5fl4VtuSoVQURDYNpnNH2upESXnMXa02Gy3VAZhTherpljiwknz9-tR1d-2oqUJzejQJQ7vqXS4SlJ3w3MxEXoDGBbstisQ85zQwu8\/w612-h640\/image.png\" width=\"612\" \/\u003E\u003C\/a\u003E\u003C\/td\u003E\u003C\/tr\u003E\u003Ctr\u003E\u003Ctd class=\"tr-caption\" style=\"text-align: justify;\"\u003E\u003Cdiv style=\"text-align: justify;\"\u003EGambar 6.\u0026nbsp;Diagram pseudoadiabatik lengkap. Terlihat bahwa p meningkat ke bawah dan digambarkan pada skala yang distorsi (mewakili \\(p^{0.286}\\)).\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003EHanya area yang berwarna biru yang umumnya dicetak untuk digunakan dalam perhitungan meteorologi. Garis-garis miring, masing-masing diberi label dengan nilai temperatur potensial \\( \\theta \\), adalah adiabatik kering.\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003ESesuai dengan definisi \\( \\theta \\), suhu aktual udara (diberikan pada absis) pada tekanan 1000 hPa sama dengan suhu potensialnya.\u003C\/div\u003E\u003C\/td\u003E\u003C\/tr\u003E\u003C\/tbody\u003E\u003C\/table\u003E\u003Cdiv style=\"text-align: justify;\"\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv class=\"separator\" style=\"clear: both; text-align: justify;\"\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003EWilayah diagram yang paling menarik dalam atmosfer adalah bagian yang ditunjukkan dalam garis putus-putus di Gambar 6, dan ini umumnya merupakan satu-satunya bagian dari diagram yang dicetak.\u003C\/div\u003E\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003EDalam diagram pseudoadiabatik, isoterma bersifat vertikal, dan adiabatik kering (θ konstan) berorientasi pada sudut tajam relatif terhadap isoterma (Gambar 6).\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003EKarena perubahan suhu dengan ketinggian di atmosfer umumnya terletak antara isotermal dan adiabatik kering, sebagian besar pembacaan suhu berada dalam rentang sempit sudut ketika digambarkan pada diagram pseudoadiabatik.\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003E\u003Cdiv style=\"text-align: justify;\"\u003EPembatasan ini diatasi dalam diagram \\(skew\\ T-ln\\ p\\), di mana ordinat (\\(y\\)) adalah \\(-ln\\ p\\) (tanda minus memastikan bahwa tingkat tekanan yang lebih rendah terletak di atas tingkat tekanan yang lebih tinggi pada diagram) dan absis (\\(x\\)) adalah:\u003C\/div\u003E\u0026nbsp;\u003C\/div\u003E\u003C\/div\u003E\u003Cspan\u003E\u0026nbsp;\u0026nbsp; \u0026nbsp;\u003C\/span\u003E\\(x = T\\ (constant)\\ y \\)\u003Cbr \/\u003E\u003Cspan\u003E\u0026nbsp;\u0026nbsp; \u0026nbsp;\u003C\/span\u003E\\(x = T - (constant)\\ ln\\ p \\)\u003Cdiv style=\"text-align: right;\"\u003E(56)\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003EMaka, akan kita dapatkan juga:\u003C\/div\u003E\u003Cdiv\u003E\\[y=\\frac{x-T}{contant}\\]\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003E\u003Cdiv style=\"text-align: justify;\"\u003EDan, untuk isoterma \\(T\\) yang konstan, hubungan antara \\(y\\) dan \\(x\\) untuk isoterma memiliki bentuk \\(y = mx + c\\), di mana \\(m\\) sama untuk semua isoterma dan \\(c\\) adalah konstanta yang berbeda untuk setiap isoterma.\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003EOleh karena itu, pada diagram \\(skew\\ T-ln\\ p\\), isoterma adalah garis lurus sejajar yang miring dari kiri ke kanan. Skala untuk sumbu \\(x\\)\u0026nbsp;umumnya dipilih agar sudut antara isoterma dan isobar sekitar 45°, seperti yang digambarkan secara skematis dalam Gambar 7.\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv\u003E\u003Ctable align=\"center\" cellpadding=\"0\" cellspacing=\"0\" class=\"tr-caption-container\" style=\"margin-left: auto; margin-right: auto;\"\u003E\u003Ctbody\u003E\u003Ctr\u003E\u003Ctd style=\"text-align: center;\"\u003E\u003Ca href=\"https:\/\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEh50400zZ97YiDMdgLsyGvZitZ38SVb_hVuahDlnhJg9_lsSXFfQu1D5zt2t78jW-Os0XjL1Iz4RLc4lm7L7Fkq3ZqQfqt1VCjadv1ynYQfsBVCj9WAuugQbrCEKJte2hoNI4RHW6M3-ylIKucUjAZB8z5GQ5CfbtVaU6l0eIF60uERYBPSMLZGdcxz44s\/s847\/image.png\" style=\"margin-left: auto; margin-right: auto;\"\u003E\u003Cimg border=\"0\" data-original-height=\"424\" data-original-width=\"847\" height=\"320\" src=\"https:\/\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEh50400zZ97YiDMdgLsyGvZitZ38SVb_hVuahDlnhJg9_lsSXFfQu1D5zt2t78jW-Os0XjL1Iz4RLc4lm7L7Fkq3ZqQfqt1VCjadv1ynYQfsBVCj9WAuugQbrCEKJte2hoNI4RHW6M3-ylIKucUjAZB8z5GQ5CfbtVaU6l0eIF60uERYBPSMLZGdcxz44s\/w640-h320\/image.png\" width=\"640\" \/\u003E\u003C\/a\u003E\u003C\/td\u003E\u003C\/tr\u003E\u003Ctr\u003E\u003Ctd class=\"tr-caption\" style=\"text-align: center;\"\u003EGambar 7.\u0026nbsp;Skema dari sebagian diagram \\(skew\\ T-ln\\ p\\)\u003C\/td\u003E\u003C\/tr\u003E\u003C\/tbody\u003E\u003C\/table\u003E\u003Cdiv class=\"separator\" style=\"clear: both; text-align: center;\"\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003EDapat dilihat bahwa isoterma pada diagram \\(skew\\ T-ln\\ p\\)\u0026nbsp;condong sekitar 45° dari orientasi vertikal pada diagram pseudoadiabatik, oleh karena itu dinamakan diagram \\(skew\\ T-ln\\ p\\).\u003C\/div\u003E\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003EDari persamaan (55), persamaan untuk adiabatik kering (\\( \\theta \\) konstan) adalah:\u003C\/div\u003E\u003Cdiv\u003E\u003Cspan\u003E\u0026nbsp;\u0026nbsp; \u0026nbsp;\u003C\/span\u003E\\(- \\ln p = const \\ln T + const\\)\u003C\/div\u003E\u003Cdiv\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003EOleh karena itu, pada diagram \\(- ln\\ p\\) versus \\(ln\\ T\\), adiabatik kering akan menjadi garis lurus.\u0026nbsp;\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003EKarena \\(-ln\\ p\\) adalah ordinat pada diagram \\(skew\\ T - ln\\ p\\), tetapi absisnya bukan \\(ln\\ T\\), adiabatik kering pada diagram ini adalah garis yang sedikit melengkung dari kanan bawah ke kiri atas.\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003ESudut antara isoterma dan adiabatik kering pada diagram \\(skew\\ T - ln\\ p\\)sekitar 90° (Gambar 7).\u0026nbsp;\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003E\u003Cbr \/\u003E\u003C\/div\u003E\u003Cdiv style=\"text-align: justify;\"\u003EOleh karena itu, ketika pembacaan suhu atmosfer dipetakan pada diagram ini, perbedaan kecil dalam kemiringan lebih tampak dibandingkan dengan pada diagram pseudoadiabatik.\u003C\/div\u003E\u003C\/div\u003E\u003C\/div\u003E\u003C\/div\u003E      \n\u003C!--batas konten--\u003E\n\u003Cdiv class=\"separator\" style=\"clear: both;\"\u003E\u003C\/div\u003E"},"link":[{"rel":"replies","type":"application/atom+xml","href":"https:\/\/www.climate4life.info\/feeds\/6387086034618372383\/comments\/default","title":"Post Comments"},{"rel":"replies","type":"text/html","href":"https:\/\/www.climate4life.info\/2023\/10\/diagram-skewT-termodinamika-atmosfer.html#comment-form","title":"0 Comments"},{"rel":"edit","type":"application/atom+xml","href":"https:\/\/www.blogger.com\/feeds\/8493873891004150846\/posts\/default\/6387086034618372383"},{"rel":"self","type":"application/atom+xml","href":"https:\/\/www.blogger.com\/feeds\/8493873891004150846\/posts\/default\/6387086034618372383"},{"rel":"alternate","type":"text/html","href":"https:\/\/www.climate4life.info\/2023\/10\/diagram-skewT-termodinamika-atmosfer.html","title":"Diagram Termodinamika Skew T-ln P"}],"author":[{"name":{"$t":"Climate4life"},"uri":{"$t":"http:\/\/www.blogger.com\/profile\/03747017448251208612"},"email":{"$t":"noreply@blogger.com"},"gd$image":{"rel":"http://schemas.google.com/g/2005#thumbnail","width":"32","height":"32","src":"\/\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEivPePtjvrBk-yk7PLc_-MxpFKrGyM63_X5n1NnKYYGCGsw6YWNSAh3eW6mN7fz8wGOCh9oNWmDri47Uu8BbHhvJLPgviz1B8QvVLZFCWmwpgoO5Wwe0J7a0lRKl3-iEJHdEsnJzL5vA1-s9OhbowA0eiTS8fuJYeMICtcF0gLouAo\/s220\/3.png"}}],"media$thumbnail":{"xmlns$media":"http://search.yahoo.com/mrss/","url":"https:\/\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEjmTaHzqohI70nqzY2_C6LKgvkO2trmnYlur3qQCsJE7ea02gaSLTfI2p4GnPBU4E84l7sl80e7oBBiiT7j7oH6StMzCLM0N4K5DI6k_533vK0am87aLkkJ6NuT9ExicpGqXWDmzsPFi5lICG-qY7iDsfroXP5p0neR7K-C2izZ7k0bO0Y6okg0BTgnTto\/s72-c\/fisika%20atmosfer%20-%20termodinamika%20awan%20dan%20hujan.png","height":"72","width":"72"},"thr$total":{"$t":"0"}}]}});