Translations:Niederschlag-Abfluss-Modell/2/en - Versionsgeschichte

Froehlich am 25. November 2020 um 08:03 Uhr

2020-11-25T08:03:06Z

← Nächstältere Version		Version vom 25. November 2020, 10:03 Uhr
Zeile 1:		Zeile 1:
	A rainfall-runoff model calculates the water balance of a hydrological catchment area. The most important output is the runoff at the outlet of the catchment area in response to the precipitation in the catchment area. The simulation can be event-based or continuous.		A rainfall-runoff model calculates the water balance of a hydrological catchment area. The most important output is the runoff at the outlet of the catchment area in response to the precipitation in the catchment area. The simulation can be event-based or continuous.
	In Talsim-NG the rainfall-runoff module is integrated into the [[Special:MyLanguage/Einzugsgebiet\|~~Sub~~-basin]] system element. Basically, all relevant physical processes of water storage and movement within the catchment area can be modeled (evaporation, snow accumulation and melting, soil moisture, etc.).		In Talsim-NG the rainfall-runoff module is integrated into the [[Special:MyLanguage/Einzugsgebiet\|sub-basin]] system element. Basically, all relevant physical processes of water storage and movement within the catchment area can be modeled (evaporation, snow accumulation and melting, soil moisture, etc.).
	Different calculation approaches are implemented and allow, depending on the given problem and data situation, to choose from simple, strongly abstracted approaches (e.g. discharge coefficient method) up to complex physically based approaches (e.g. [[Special:MyLanguage/Einzugsgebiet#Bodenfeuchtesimulation\|~~Soil~~ moisture simulation]]).		Different calculation approaches are implemented and allow, depending on the given problem and data situation, to choose from simple, strongly abstracted approaches (e.g. discharge coefficient method) up to complex physically based approaches (e.g. [[Special:MyLanguage/Einzugsgebiet#Bodenfeuchtesimulation\|soil moisture simulation]]).
	A detailed description of the calculation approaches can be found directly on the page of the [[Special:MyLanguage/Einzugsgebiet\|~~Sub~~-basin]] system element.		A detailed description of the calculation approaches can be found directly on the page of the [[Special:MyLanguage/Einzugsgebiet\|sub-basin]] system element.

Froehlich am 25. November 2020 um 08:02 Uhr

2020-11-25T08:02:38Z

← Nächstältere Version		Version vom 25. November 2020, 10:02 Uhr
Zeile 1:		Zeile 1:
	~~In a~~ rainfall-runoff model the water balance of a hydrological catchment area ~~is calculated~~. The most important output is the runoff at the outlet of the catchment area in response to the ~~areal~~ precipitation ~~fallen~~ in the catchment area. The ~~consideration~~ can be event-based or continuous.		A rainfall-runoff model calculates the water balance of a hydrological catchment area. The most important output is the runoff at the outlet of the catchment area in response to the precipitation in the catchment area. The simulation can be event-based or continuous.
	In Talsim-NG the ~~precipitation~~-runoff ~~model~~ is integrated into the ~~system element~~ [[Special:MyLanguage/Einzugsgebiet\|~~Catchment Area~~]]. Basically, all ~~essential~~ physical processes of water storage and movement within the catchment area can be modeled (evaporation, snow accumulation and melting, soil moisture, etc.).		In Talsim-NG the rainfall-runoff module is integrated into the [[Special:MyLanguage/Einzugsgebiet\|Sub-basin]] system element. Basically, all relevant physical processes of water storage and movement within the catchment area can be modeled (evaporation, snow accumulation and melting, soil moisture, etc.).
	Different calculation approaches are implemented and allow, depending on the given problem and data situation, to choose from simple, strongly abstracted approaches (e.g. discharge coefficient method) up to complex physically based approaches (e.g. [[Special:MyLanguage/Einzugsgebiet#Bodenfeuchtesimulation\|Soil ~~Moisture Simulation~~]]).		Different calculation approaches are implemented and allow, depending on the given problem and data situation, to choose from simple, strongly abstracted approaches (e.g. discharge coefficient method) up to complex physically based approaches (e.g. [[Special:MyLanguage/Einzugsgebiet#Bodenfeuchtesimulation\|Soil moisture simulation]]).
	A detailed description of the calculation approaches can be found directly on the page of the ~~system element~~ [[Special:MyLanguage/Einzugsgebiet\|~~Catchment Area~~]].		A detailed description of the calculation approaches can be found directly on the page of the [[Special:MyLanguage/Einzugsgebiet\|Sub-basin]] system element.

Ferrao am 7. Oktober 2020 um 11:18 Uhr

2020-10-07T11:18:12Z

← Nächstältere Version		Version vom 7. Oktober 2020, 13:18 Uhr
Zeile 1:		Zeile 1:
	In a rainfall-runoff model the water balance of a hydrological catchment area is calculated. The most important output is the runoff at the outlet of the catchment area in response to the areal precipitation fallen in the catchment area. The consideration can be event-based or continuous.		In a rainfall-runoff model the water balance of a hydrological catchment area is calculated. The most important output is the runoff at the outlet of the catchment area in response to the areal precipitation fallen in the catchment area. The consideration can be event-based or continuous.
	In Talsim-NG the precipitation-runoff model is integrated into the system element [[Special:MyLanguage/Einzugsgebiet\|Catchment Area]]. Basically, all essential physical processes of water storage and movement within the catchment area can be modeled (evaporation, snow accumulation and melting, soil moisture, etc.).		In Talsim-NG the precipitation-runoff model is integrated into the system element [[Special:MyLanguage/Einzugsgebiet\|Catchment Area]]. Basically, all essential physical processes of water storage and movement within the catchment area can be modeled (evaporation, snow accumulation and melting, soil moisture, etc.).
	Different calculation approaches are implemented and allow, depending on the given problem and data situation, to choose from simple, strongly abstracted approaches (e.g. discharge coefficient method) up to complex physically based approaches (e.g. [[Special:MyLanguage/Einzugsgebiet#Bodenfeuchtesimulation\|Soil Moisture Simulation]].		Different calculation approaches are implemented and allow, depending on the given problem and data situation, to choose from simple, strongly abstracted approaches (e.g. discharge coefficient method) up to complex physically based approaches (e.g. [[Special:MyLanguage/Einzugsgebiet#Bodenfeuchtesimulation\|Soil Moisture Simulation]]).
	A detailed description of the calculation approaches can be found directly on the page of the system element [[Special:MyLanguage/Einzugsgebiet\|Catchment Area]].		A detailed description of the calculation approaches can be found directly on the page of the system element [[Special:MyLanguage/Einzugsgebiet\|Catchment Area]].

Ferrao am 7. Oktober 2020 um 09:37 Uhr

2020-10-07T09:37:20Z

← Nächstältere Version		Version vom 7. Oktober 2020, 11:37 Uhr
Zeile 2:		Zeile 2:
	In Talsim-NG the precipitation-runoff model is integrated into the system element [[Special:MyLanguage/Einzugsgebiet\|Catchment Area]]. Basically, all essential physical processes of water storage and movement within the catchment area can be modeled (evaporation, snow accumulation and melting, soil moisture, etc.).		In Talsim-NG the precipitation-runoff model is integrated into the system element [[Special:MyLanguage/Einzugsgebiet\|Catchment Area]]. Basically, all essential physical processes of water storage and movement within the catchment area can be modeled (evaporation, snow accumulation and melting, soil moisture, etc.).
	Different calculation approaches are implemented and allow, depending on the given problem and data situation, to choose from simple, strongly abstracted approaches (e.g. discharge coefficient method) up to complex physically based approaches (e.g. [[Special:MyLanguage/Einzugsgebiet#Bodenfeuchtesimulation\|Soil Moisture Simulation]].		Different calculation approaches are implemented and allow, depending on the given problem and data situation, to choose from simple, strongly abstracted approaches (e.g. discharge coefficient method) up to complex physically based approaches (e.g. [[Special:MyLanguage/Einzugsgebiet#Bodenfeuchtesimulation\|Soil Moisture Simulation]].
	A detailed description of the calculation approaches can be found directly on the page of the system element [[Special:MyLanguage/~~Catchment Area~~\|Catchment Area]].		A detailed description of the calculation approaches can be found directly on the page of the system element [[Special:MyLanguage/Einzugsgebiet\|Catchment Area]].

Ferrao am 7. Oktober 2020 um 09:29 Uhr

2020-10-07T09:29:03Z

← Nächstältere Version		Version vom 7. Oktober 2020, 11:29 Uhr
Zeile 1:		Zeile 1:
	In a rainfall-runoff model the water balance of a hydrological catchment area is calculated. The most important output is the runoff at the outlet of the catchment area in response to the areal precipitation fallen in the catchment area. The consideration can be event-based or continuous.		In a rainfall-runoff model the water balance of a hydrological catchment area is calculated. The most important output is the runoff at the outlet of the catchment area in response to the areal precipitation fallen in the catchment area. The consideration can be event-based or continuous.
	In Talsim-NG the precipitation-runoff model is integrated into the system element [[Special:MyLanguage/Einzugsgebiet\|Catchment Area]]. Basically, all essential physical processes of water storage and movement within the catchment area can be modeled (evaporation, snow accumulation and melting, soil moisture, etc.).		In Talsim-NG the precipitation-runoff model is integrated into the system element [[Special:MyLanguage/Einzugsgebiet\|Catchment Area]]. Basically, all essential physical processes of water storage and movement within the catchment area can be modeled (evaporation, snow accumulation and melting, soil moisture, etc.).
	Different calculation approaches are implemented and allow, depending on the given problem and data situation, to choose from simple, strongly abstracted approaches (e.g. discharge coefficient method) up to complex physically based approaches (e.g. [[Special:MyLanguage/~~Catchment Area~~#~~Soil Moisture Simulation~~\|Soil Moisture Simulation]].		Different calculation approaches are implemented and allow, depending on the given problem and data situation, to choose from simple, strongly abstracted approaches (e.g. discharge coefficient method) up to complex physically based approaches (e.g. [[Special:MyLanguage/Einzugsgebiet#Bodenfeuchtesimulation\|Soil Moisture Simulation]].
	A detailed description of the calculation approaches can be found directly on the page of the system element [[Special:MyLanguage/Catchment Area\|Catchment Area]].		A detailed description of the calculation approaches can be found directly on the page of the system element [[Special:MyLanguage/Catchment Area\|Catchment Area]].

Ferrao: Die Seite wurde neu angelegt: „In a rainfall-runoff model the water balance of a hydrological catchment area is calculated. The most important output is the runoff at the outlet of the catch…“

2020-10-07T09:22:55Z

Die Seite wurde neu angelegt: „In a rainfall-runoff model the water balance of a hydrological catchment area is calculated. The most important output is the runoff at the outlet of the catch…“

Neue Seite

In a rainfall-runoff model the water balance of a hydrological catchment area is calculated. The most important output is the runoff at the outlet of the catchment area in response to the areal precipitation fallen in the catchment area. The consideration can be event-based or continuous.
In Talsim-NG the precipitation-runoff model is integrated into the system element [[Special:MyLanguage/Einzugsgebiet|Catchment Area]]. Basically, all essential physical processes of water storage and movement within the catchment area can be modeled (evaporation, snow accumulation and melting, soil moisture, etc.).
Different calculation approaches are implemented and allow, depending on the given problem and data situation, to choose from simple, strongly abstracted approaches (e.g. discharge coefficient method) up to complex physically based approaches (e.g. [[Special:MyLanguage/Catchment Area#Soil Moisture Simulation|Soil Moisture Simulation]].
A detailed description of the calculation approaches can be found directly on the page of the system element [[Special:MyLanguage/Catchment Area|Catchment Area]].