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hydrology$36463$ - translation to german
![terrain map]] of the [[Latorița River]]'s drainage basin in [[Romania]]](https://commons.wikimedia.org/wiki/Special:FilePath/EN Bazinul hidrografic al Raului Latorita, Romania.jpg?width=200 "terrain map]] of the [[Latorița River]]'s drainage basin in [[Romania]]")
![dendritic]] drainage basin. The dashed line is the main water divide of the [[hydrography]] basin.](https://commons.wikimedia.org/wiki/Special:FilePath/Hydrographic basin.svg?width=200 "dendritic]] drainage basin. The dashed line is the main water divide of the [[hydrography]] basin.")
![[[Digital terrain model]] of the Latorița River's drainage basin in [[Romania]].](https://commons.wikimedia.org/wiki/Special:FilePath/Modelare 3D pentru Bazinul Hidrografic al Paraului Latorita.gif?width=200 "[[Digital terrain model]] of the Latorița River's drainage basin in [[Romania]].")
![Major [[continental divide]]s, showing how terrestrial drainage basins drain into the oceans. Grey areas are [[endorheic basin]]s that do not drain to the oceans](https://commons.wikimedia.org/wiki/Special:FilePath/Ocean drainage.png?width=200 "Major [[continental divide]]s, showing how terrestrial drainage basins drain into the oceans. Grey areas are [[endorheic basin]]s that do not drain to the oceans")
![Drainage basin of the [[Ohio River]], part of the [[Mississippi River]] drainage basin](https://commons.wikimedia.org/wiki/Special:FilePath/Ohiorivermap.png?width=200 "Drainage basin of the [[Ohio River]], part of the [[Mississippi River]] drainage basin")
![[[Endorheic basin]] in [[Central Asia]]](https://commons.wikimedia.org/wiki/Special:FilePath/Uureg Nuur.jpg?width=200 "[[Endorheic basin]] in [[Central Asia]]")
Wikipedia
Geographic information systems (GISs) have become a useful and important tool in the field of hydrology to study and manage Earth's water resources. Climate change and greater demands on water resources require a more knowledgeable disposition of arguably one of our most vital resources. Because water in its occurrence varies spatially and temporally throughout the hydrologic cycle, its study using GIS is especially practical. Whereas previous GIS systems were mostly static in their geospatial representation of hydrologic features, GIS platforms are becoming increasingly dynamic, narrowing the gap between historical data and current hydrologic reality.
The elementary water cycle has inputs equal to outputs plus or minus change in storage. Hydrologists make use of this hydrologic budget when they study a watershed. The inputs in a hydrologic budget include precipitation, surface flow, and groundwater flow. Outputs consist of evapotranspiration, infiltration, surface runoff, and surface/groundwater flows. All of these quantities can be measured or estimated based on environmental data and their characteristics can be graphically displayed and studies using GIS.
