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Im Gegensatz zu anderen Wasserhaushaltsgrößen kann die GWN in der Regel nicht direkt gemessen werden. Der Anwendung entsprechender Modelle kommt daher eine besondere Bedeutung zu. \\n\\nDie hier zur Verfügung gestellten Daten der GWN stammen aus der landesweiten Langzeit-Berechnung mit dem Bodenwasserhaushaltsmodell GWN-BW. GWN-BW ist ein modular aufgebautes, deterministisches und flächendifferenziertes Modell zur Berechnung der tatsächlichen Verdunstung, zur Simulation des Bodenwasserhaushaltes und der unterhalb der durchwurzelten Bodenzone gebildeten Sickerwassermenge. Wie die meisten vergleichbaren Wasserhaushaltsmodelle benötigt GWN-BW als meteorologischen Antrieb Daten der Niederschlagshöhe, der Lufttemperatur, der relativen Luftfeuchte, der Globalstrahlung oder Sonnenscheindauer sowie der Windstärke oder –geschwindigkeit. \"},{\"attributes\":{\"cadenza-link\":{\"popupMaximized\":false,\"url\":\"https://www.hydrosconsult.com/hydrologie/bodenwasserhaushalt\",\"linkTarget\":\"NEW_WINDOW\",\"type\":\"static\",\"invalid\":\"false\",\"transferConditionMode\":\"NONE\",\"transferSelectionAsFilter\":false,\"showLinkIcon\":false}},\"insert\":\"https://www.hydrosconsult.com/hydrologie/bodenwasserhaushalt\"},{\"insert\":\"\\n\\nDie Berechnungen erfolgen auf insgesamt 102.677 Grundflächen, deren Geometrie auf der Verschneidung von Bodenkarte 1:50.000 und CORINE 2006 Landnutzung beruht.\\nBei der GWN handelt sich um eine berechnete Bilanzkomponente, welche dem Gesamtabfluss abzüglich schneller lateraler Abflusskomponenten entspricht. Der Direktabfluss wird mit Hilfe des regionalisierten Baseflow-Index berücksichtigt. Die berechnete GWN entspricht jener des jeweils obersten Grundwasserstockwerks. Dies können auch hängende Grundwasserleiter sein, die beispielsweise wieder über Quellen entwässern. Sie entspricht somit, je nach den hydrogeologischen Bedingungen, nicht zwingend der GWN des obersten Hauptgrundwasserleiters.\\n\\nDie GWN kann in Folge von kapillarem Aufstieg negativ werden. Kapillarer Aufstieg wird berechnet wo die Bodenkarte grundwasserbeeinflusste Böden ausweist und ggf. vorhandene Gleichenpläne einen entsprechend geringen Flurabstand anzeigen und nicht unter landwirtschaftlicher Nutzung allgemein von Drainage ausgegangen wird.\\n\\nIm Karst (Oberjura, Muschelkalk) können auch schnelle Abflusskomponenten den Grundwasserkörper durchlaufen. Dort beschreibt die Bilanzgröße GWN nur den zeitlich verzögert zum Abfluss kommenden, als wasserwirtschaftlich nutzbar aufgefassten Teil der Wasserumsätze im Grundwasser, während die Sickerwasserrate in solchen Gebieten der gesamten Grundwasserneubildung entspricht.\\n\\n\"},{\"attributes\":{\"size\":\"large\",\"bold\":true},\"insert\":\"Aggregierte Daten als Karte und Diagramm\"},{\"insert\":\"\\nDie Daten der Grundflächen wurden auf Gemeinde- und Kreisebene aggregiert. \\nDas Arbeitsblatt \"},{\"attributes\":{\"cadenza-link\":{\"invalid\":\"false\",\"popupMaximized\":false,\"transferSelectionAsFilter\":false,\"transferConditionMode\":\"NONE\",\"worksheetId\":\"B8U1FhGVx5Dl4NMfjdRT\",\"repositoryName\":\"uheTjYRE9KZO8qEFtRqq\",\"workbookName\":\"DKLTp6Oz7qU8LLiGi9ob\",\"linkTarget\":\"CURRENT_WINDOW\",\"type\":\"worksheet\",\"showLinkIcon\":false}},\"insert\":\"Karte\"},{\"insert\":\" zeigt die räumliche Verteilung der über die letzten 30 Jahre gemittelten aggregierten Werte der Grundwasserneubildung pro Jahr auf Stadt- und Landkreisebene. Durch Hineinzoomen in die Karte wird die Aggregation auf Gemeindeebene eingeblendet. \\nDie Arbeitsblätter \"},{\"attributes\":{\"cadenza-link\":{\"popupMaximized\":false,\"transferSelectionAsFilter\":false,\"transferConditionMode\":\"NONE\",\"worksheetId\":\"vkYMNySKxKynDLR__QP7\",\"repositoryName\":\"uheTjYRE9KZO8qEFtRqq\",\"workbookName\":\"DKLTp6Oz7qU8LLiGi9ob\",\"linkTarget\":\"CURRENT_WINDOW\",\"type\":\"worksheet\",\"invalid\":\"false\",\"showLinkIcon\":false}},\"insert\":\"Aggregierte Daten pro Kreis\"},{\"insert\":\" und \"},{\"attributes\":{\"cadenza-link\":{\"popupMaximized\":false,\"transferSelectionAsFilter\":false,\"transferConditionMode\":\"NONE\",\"worksheetId\":\"bDa3HYAl7YUNbzguB-43\",\"repositoryName\":\"uheTjYRE9KZO8qEFtRqq\",\"workbookName\":\"DKLTp6Oz7qU8LLiGi9ob\",\"linkTarget\":\"CURRENT_WINDOW\",\"type\":\"worksheet\",\"invalid\":\"false\",\"showLinkIcon\":false}},\"insert\":\"Aggregierte Daten pro Gemeinde\"},{\"insert\":\" zeigen die zeitliche Verteilung der Aggregierten Werte als Tabelle und Diagramm. Über das Export-Symbol über den Tabellen können die Daten als CSV oder Excel-Datei exportiert werden.\\n \\n\"},{\"attributes\":{\"size\":\"large\",\"bold\":true},\"insert\":\"Export der Grundflächen und Einzelwerte\"},{\"insert\":\"\\nIm Arbeitsblatt \"},{\"attributes\":{\"cadenza-link\":{\"popupMaximized\":false,\"transferSelectionAsFilter\":false,\"transferConditionMode\":\"NONE\",\"worksheetId\":\"UN1gcuSkVLNZMaDzLLDY\",\"repositoryName\":\"uheTjYRE9KZO8qEFtRqq\",\"workbookName\":\"DKLTp6Oz7qU8LLiGi9ob\",\"linkTarget\":\"CURRENT_WINDOW\",\"type\":\"worksheet\",\"invalid\":\"false\",\"showLinkIcon\":false}},\"insert\":\"Grundflächen\"},{\"insert\":\" können die Grundflächen, sowie die Einzeljahreswerte und die Dreissigjahreswerte heruntergeladen werden.\\nZunächst ist ein Stadt- oder Landkreis, sowie optional eine oder mehrere Gemeinden auszuwählen.\\nÜber das Export-Symbol über den beiden Tabellen können die Daten als CSV oder Excel-Datei exportiert werden\"},{\"attributes\":{\"list\":\"bullet\"},\"insert\":\"\\n\"},{\"insert\":\"In der Karte können über das Dreipunktmenü in der Legende und den Menüpunkt Export die Geometrien als Shapefile oder KML exportiert werden\"},{\"attributes\":{\"list\":\"bullet\"},\"insert\":\"\\n\"},{\"insert\":\".\\n\"}]}","text.content.default":"","image.scale.default":"contain","text.title":"Grundwasserneubildung aus Niederschlag (GWN); Dimension: mm/Jahr:\nUnter den Bilanzgrößen des 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