1.0Hidrologihttps://hidrologi.net/wikidoelxyzhttps://hidrologi.net/wiki/author/doelxyz/rich600338<blockquote class="wp-embedded-content" data-secret="2KJJNsYV5k"><a href="https://hidrologi.net/wiki/tipe-hujan/">Tipe Hujan</a></blockquote><iframe sandbox="allow-scripts" security="restricted" src="https://hidrologi.net/wiki/tipe-hujan/embed/#?secret=2KJJNsYV5k" width="600" height="338" title="“Tipe Hujan” — Hidrologi" data-secret="2KJJNsYV5k" frameborder="0" marginwidth="0" marginheight="0" scrolling="no" class="wp-embedded-content"></iframe><script> /*! This file is auto-generated */ !function(d,l){"use strict";l.querySelector&&d.addEventListener&&"undefined"!=typeof URL&&(d.wp=d.wp||{},d.wp.receiveEmbedMessage||(d.wp.receiveEmbedMessage=function(e){var t=e.data;if((t||t.secret||t.message||t.value)&&!/[^a-zA-Z0-9]/.test(t.secret)){for(var s,r,n,a=l.querySelectorAll('iframe[data-secret="'+t.secret+'"]'),o=l.querySelectorAll('blockquote[data-secret="'+t.secret+'"]'),c=new RegExp("^https?:$","i"),i=0;i<o.length;i++)o[i].style.display="none";for(i=0;i<a.length;i++)s=a[i],e.source===s.contentWindow&&(s.removeAttribute("style"),"height"===t.message?(1e3<(r=parseInt(t.value,10))?r=1e3:~~r<200&&(r=200),s.height=r):"link"===t.message&&(r=new URL(s.getAttribute("src")),n=new URL(t.value),c.test(n.protocol))&&n.host===r.host&&l.activeElement===s&&(d.top.location.href=t.value))}},d.addEventListener("message",d.wp.receiveEmbedMessage,!1),l.addEventListener("DOMContentLoaded",function(){for(var e,t,s=l.querySelectorAll("iframe.wp-embedded-content"),r=0;r<s.length;r++)(t=(e=s[r]).getAttribute("data-secret"))||(t=Math.random().toString(36).substring(2,12),e.src+="#?secret="+t,e.setAttribute("data-secret",t)),e.contentWindow.postMessage({message:"ready",secret:t},"*")},!1)))}(window,document); //# sourceURL=https://hidrologi.net/wiki/wp-includes/js/wp-embed.min.js </script> Hujan terjadi ketika udara basah naik ke atmosfer, mengalami pendinginan, dan kemudian terjadi kondensasi yang menghasilkan butiran air atau es yang jatuh sebagai hujan. Berdasarkan mekanisme naiknya udara ke atas, hujan dapat dibedakan menjadi hujan konvektif, hujan siklonik, dan hujan orografis. 1. Hujan Konvektif Hujan konvektif terjadi akibat pemanasan intensif di permukaan tanah, terutama di […]https://hidrologi.net/wiki/wp-content/uploads/2025/02/image.png684456