{"version":"1.0","provider_name":"matforge.org","provider_url":"https:\/\/matforge.org","author_name":"Elena Markovska","author_url":"https:\/\/matforge.org\/author\/elena-markovska\/","title":"Geophysik-Anwendungen: PDE-Modellierung f\u00fcr Erdsysteme - matforge.org","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"3e1wyslvj9\"><a href=\"https:\/\/matforge.org\/de\/geophysics-applications-pde-modeling-for-earth-systems\/\">Geophysik-Anwendungen: PDE-Modellierung f\u00fcr Erdsysteme<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/matforge.org\/de\/geophysics-applications-pde-modeling-for-earth-systems\/embed\/#?secret=3e1wyslvj9\" width=\"600\" height=\"338\" title=\"&#8222;Geophysik-Anwendungen: PDE-Modellierung f\u00fcr Erdsysteme&#8220; &#8211; matforge.org\" data-secret=\"3e1wyslvj9\" frameborder=\"0\" marginwidth=\"0\" marginheight=\"0\" scrolling=\"no\" class=\"wp-embedded-content\"><\/iframe><script>\n\/*! This file is auto-generated *\/\n!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);\n\/\/# sourceURL=https:\/\/matforge.org\/wp-includes\/js\/wp-embed.min.js\n<\/script>\n","description":"Geophysikalische Ph\u00e4nomene &#8211; von der Grundwasserstr\u00f6mung zur Mantelkonvektion &#8211; werden durch partielle Differentialgleichungen (PDES) bestimmt. Finite Volume-Methoden (FVM) l\u00f6sen diese PDEs, indem sie die Erhaltungsgesetze \u00fcber Kontrollvolumen durchsetzen und sie ideal f\u00fcr komplexe, nichtlineare Erdsysteme sind. Python-Tools wie FIPY bieten flexible PDE-L\u00f6sungsfunktionen, w\u00e4hrend dom\u00e4nenspezifische Pakete wie Modflow\/Flopy standardisierte Workflows f\u00fcr die Grundwassermodellierung bieten. W\u00e4hlen Sie [&hellip;]"}