{"id":20479,"date":"2021-08-15T13:39:50","date_gmt":"2021-08-15T05:39:50","guid":{"rendered":"https:\/\/atmgeo.pccu.edu.tw\/asWeb\/?post_type=course&#038;p=20479"},"modified":"2024-04-20T16:33:22","modified_gmt":"2024-04-20T08:33:22","slug":"%e8%bf%91%e5%9c%b0%e9%9d%a2%e5%be%ae%e6%b0%a3%e8%b1%a1%e5%ad%b8","status":"publish","type":"course","link":"https:\/\/atmgeo.pccu.edu.tw\/asWeb\/course\/%e8%bf%91%e5%9c%b0%e9%9d%a2%e5%be%ae%e6%b0%a3%e8%b1%a1%e5%ad%b8\/","title":{"rendered":"\u8fd1\u5730\u9762\u5fae\u6c23\u8c61\u5b78"},"content":{"rendered":"\n<p>\u8fd1\u5730\u9762\u5fae\u6c23\u8c61\u5b78\u662f\u5728\u63a2\u8a0e\u767c\u751f\u5728\u5927\u6c23\u908a\u754c\u5c64\uff08\u6216\u53ef\u7a31\u70ba\u884c\u661f\u908a\u754c\u5c64\uff09\u7684\u5404\u7a2e\u5927\u6c23\u73fe\u8c61\uff0c\u5728\u5927\u6c23\u908a\u754c\u5c64\u4e2d\uff0c\u5927\u6c23\u8207\u5730\u7403\u8868\u9762\u5177\u6709\u986f\u8457\u7684\u52d5\u91cf\uff0c\u8cea\u91cf\u53ca\u71b1\u91cf\u4ea4\u63db\uff0c \u800c\u5176\u89c0\u6e2c\u7279\u5fb5\u5982\u6eab\u5ea6,\u901f\u5ea6\u53ca\u5bc6\u5ea6\u5177\u6709\u9ad8\u5ea6\u7684\u8b8a\u7570\u6027\uff0c\u4e14\u9019\u4e9b\u73fe\u8c61\u4e3b\u8981\u727d\u6d89\u5230\u5c0f\u5c3a\u5ea6\u7684\u904e\u7a0b\u3002\u96d6\u7136\u5927\u6c23\u908a\u754c\u5c64\u53ea\u4f54\u5927\u6c23\u5c64\u7684\u6975\u5c0f\u90e8\u5206\u3002\u7136\u800c\u5176\u4f34\u96a8\u7684\u5c0f\u5c3a\u5ea6\u7269\u7406\u904e\u7a0b\u5c0d\u65bc\u4eba\u985e\u6d3b\u52d5\u53ca\u751f\u7269\u751f\u5b58\u6709\u91cd\u8981\u5f71\u97ff\u3002\u672c\u8ab2\u7a0b\u5167\u5bb9\u5c07\u91dd\u5c0d\u4e0b\u5217\u4e3b\u984c\u4f5c\u6709\u7cfb\u7d71\u7684\u95e1\u91cb\uff1a1.\u5fae\u6c23\u8c61\u5b78\u7c21\u4ecb 2.\u8fd1\u5730\u9762\u5c64\u7684\u80fd\u91cf\u6536\u652f 3.\u571f\u58e4\u6eab\u5ea6\u8207\u71b1\u91cf\u50b3\u9001 4.\u5927\u6c23\u908a\u754c\u5c64\u7684\u6eab\u5ea6\u8207\u6fd5\u5ea6 5.\u5927\u6c23\u908a\u754c\u5c64\u7684\u6c23\u6d41\u7279\u6027\u3002<\/p>\n\n\n\n<p>The scope of micrometeorology is limited to only those phenomena occurring in the atmospheric boundary layer (or called planetary boundary layer). Significant exchange of momentum, heat, or mass takes place between the surface and the atmospheric air. Sharp variations in the properties of the flow, such as temperature, velocity, and mass, also occur in the boundary layer. These characteristics are primarily related to the small-scale processes. Although the atmospheric boundary layer comprises only a tiny fraction of the atmosphere, its associated small-scale physical processes are important for the human activities and even survival of life on earth. The course outline will primarily include: (1) Introduction, (2) Energy Budget near the Surface, (3) Soil Temperature and Heat Transfer, (4) Air temperature and Humidity in the Atmospheric Boundary Layer, (5) Wind Distribution in the Atmospheric Boundary Layer.<\/p>\n","protected":false},"featured_media":35216,"parent":0,"template":"","meta":[],"course-classification":[839,835],"class_list":["post-20479","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\u4e8c\u5e74\u7d1a"],"subject":["\u9078\u4fee"],"professor-to-courses_from":["32031"]},"_links":{"self":[{"href":"https:\/\/atmgeo.pccu.edu.tw\/asWeb\/wp-json\/wp\/v2\/course\/20479","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\/35216"}],"wp:attachment":[{"href":"https:\/\/atmgeo.pccu.edu.tw\/asWeb\/wp-json\/wp\/v2\/media?parent=20479"}],"wp:term":[{"taxonomy":"course-classification","embeddable":true,"href":"https:\/\/atmgeo.pccu.edu.tw\/asWeb\/wp-json\/wp\/v2\/course-classification?post=20479"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}