{"id":20481,"date":"2021-08-15T13:42:27","date_gmt":"2021-08-15T05:42:27","guid":{"rendered":"https:\/\/atmgeo.pccu.edu.tw\/asWeb\/?post_type=course&#038;p=20481"},"modified":"2024-04-20T16:30:05","modified_gmt":"2024-04-20T08:30:05","slug":"%e8%a1%9b%e6%98%9f%e6%b0%a3%e8%b1%a1%e5%ad%b8","status":"publish","type":"course","link":"https:\/\/atmgeo.pccu.edu.tw\/asWeb\/course\/%e8%a1%9b%e6%98%9f%e6%b0%a3%e8%b1%a1%e5%ad%b8\/","title":{"rendered":"\u885b\u661f\u6c23\u8c61\u5b78<br>SATELLITE METEOROLOGY"},"content":{"rendered":"\n<p>\u672c\u8ab2\u7a0b\u7684\u76ee\u7684\u5728\u4f7f\u4fee\u8ab2\u540c\u5b78\u719f\u6089\u885b\u661f\u8cc7\u6599\u4e4b\u7814\u5224\u6280\u5de7\u3001\u5982\u4f55\u5f9e\u885b\u661f\u96f2\u5716\u8fa8\u8a8d\u5404\u7a2e\u5929\u6c23\u7cfb\u7d71\u4ee5\u53ca\u885b\u661f\u8cc7\u6599\u5728\u4e0d\u540c\u5929\u6c23\u7cfb\u7d71\uff08\u5982\u4e2d\u7def\u5ea6\u3001\u4e2d\u5c3a\u5ea6\u548c\u71b1\u5e36\u5929\u6c23\u7cfb\u7d71\uff09\u4e4b\u61c9\u7528\u3002\u6559\u5b78\u5167\u5bb9\u5982\u4e0b\uff1a (1)\u6c23\u8c61\u885b\u661f\u7c21\u4ecb\uff1b (2) \u885b\u661f\u8cc7\u6599\u4e4b\u7814\u5224\u6280\u5de7\uff1b(3) \u5404\u7a2e\u5929\u6c23\u7cfb\u7d71\u4e4b\u8fa8\u8a8d\uff1b(4) \u885b\u661f\u8cc7\u6599\u5728\u7d9c\u89c0\u5c3a\u5ea6 (\u5982: \u5927\u5c3a\u5ea6\u96f2\u7cfb\u4e4b\u5206\u6790\u3001\u5730\u9762\u92d2\u9762\u8207\u810a\u7dda\u3001\u9ad8\u7a7a\u69fd\u810a\u7dda\u53ca\u9ad8\u5c64\u5674\u6d41\u4e4b\u5b9a\u4f4d)\uff1b(5) \u885b\u661f\u8cc7\u6599\u5728\u4e2d\u5c3a\u5ea6\u5929\u6c23\u7cfb\u7d71\u4e4b\u61c9\u7528 (\u542b\u5f62\u6210\u8207\u52a0\u5f37\u4e4b\u6fc0\u767c\u6a5f\u5236\u3001\u79fb\u52d5\u904e\u7a0b)\uff1b(6) \u885b\u661f\u8cc7\u6599\u5728\u71b1\u5e36\u5929\u6c23\u7cfb\u7d71 (\u5982\u9ad8\u7a7a\u51b7\u6e26) \u548c\u98b1\u98a8 (\u542b\u4e2d\u5fc3\u5b9a\u4f4d\u53ca\u5f37\u5ea6\u5206\u6790\u8207\u9810\u5831)\u3002<br>The following topics are included in this course, hoping that they can benefit students on the related courses, research and the operations in the future. 1. introduction to meteorological satellite, data types and characteristics as well as the relative interpretation techniques. 2. the analyses and applications of the satellite data on different weather scales: a. synoptic weather scale, such as to analyze the large scale cloud systems, to locate the surface front band and ridge lines, upper trough and ridge lines as well as upper jet stream; b. tropical weather systems (such as cold low in upper troposphere) and typhoon (including center locations, intensity analysis and forecasting); c. mesoscale convective systems (including the trigger mechanism of initiation and intensification as well as the propagation process).<\/p>\n","protected":false},"featured_media":31938,"parent":0,"template":"","meta":[],"course-classification":[839,835],"class_list":["post-20481","course","type-course","status-publish","has-post-thumbnail","hentry","course-classification-under-severe","course-classification-under-graduate"],"meta_box":{"credits":"3","level":["\u5927\u5b78\u90e8\u4e09\u5e74\u7d1a"],"subject":["\u9078\u4fee"],"professor-to-courses_from":["35213"]},"_links":{"self":[{"href":"https:\/\/atmgeo.pccu.edu.tw\/asWeb\/wp-json\/wp\/v2\/course\/20481","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/atmgeo.pccu.edu.tw\/asWeb\/wp-json\/wp\/v2\/course"}],"about":[{"href":"https:\/\/atmgeo.pccu.edu.tw\/asWeb\/wp-json\/wp\/v2\/types\/course"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/atmgeo.pccu.edu.tw\/asWeb\/wp-json\/wp\/v2\/media\/31938"}],"wp:attachment":[{"href":"https:\/\/atmgeo.pccu.edu.tw\/asWeb\/wp-json\/wp\/v2\/media?parent=20481"}],"wp:term":[{"taxonomy":"course-classification","embeddable":true,"href":"https:\/\/atmgeo.pccu.edu.tw\/asWeb\/wp-json\/wp\/v2\/course-classification?post=20481"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}