Translations:Einzugsgebiet/30/en - Versionsgeschichte

Froehlich am 25. November 2020 um 14:57 Uhr

2020-11-25T14:57:41Z

← Nächstältere Version		Version vom 25. November 2020, 16:57 Uhr
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	Using a CN value that is dependent on the soil type and land use (see /DVWK, 1991/), the initial losses and a relationship between the runoff coefficient and the accumulated rainfall amount up to the current point in time can be derived, both of which are dependent on antecedent conditions /Zaiss, 1987/. With this approach, the runoff coefficient increases with increasing precipitation amount during the course of the rainfall event.		Using a CN value that is dependent on the soil type and land use (see /DVWK, 1991/), the initial losses and a relationship between the runoff coefficient and the accumulated rainfall amount up to the current point in time can be derived, both of which are dependent on antecedent conditions /Zaiss, 1987/. With this approach, the runoff coefficient increases with increasing precipitation amount during the course of the rainfall event.
	The quantification of the ~~previous~~ conditions is based on the 21-day-precipitation index <math>VN</math>.		The quantification of the antecedent conditions is based on the 21-day-precipitation index <math>VN</math>.

Froehlich am 25. November 2020 um 14:57 Uhr

2020-11-25T14:57:22Z

← Nächstältere Version		Version vom 25. November 2020, 16:57 Uhr
Zeile 1:		Zeile 1:
	Using a CN value that is dependent on the soil type and land use (see /DVWK, 1991/), the initial losses and a relationship between the runoff coefficient and the accumulated rainfall amount up to the current point in time can be derived, both of which are dependent on ~~previous~~ conditions /Zaiss, 1987/. With this approach, the runoff coefficient increases with increasing precipitation amount during the course of the rainfall event.		Using a CN value that is dependent on the soil type and land use (see /DVWK, 1991/), the initial losses and a relationship between the runoff coefficient and the accumulated rainfall amount up to the current point in time can be derived, both of which are dependent on antecedent conditions /Zaiss, 1987/. With this approach, the runoff coefficient increases with increasing precipitation amount during the course of the rainfall event.
	The quantification of the previous conditions is based on the 21-day-precipitation index <math>VN</math>.		The quantification of the previous conditions is based on the 21-day-precipitation index <math>VN</math>.

Froehlich am 25. November 2020 um 10:28 Uhr

2020-11-25T10:28:33Z

← Nächstältere Version		Version vom 25. November 2020, 12:28 Uhr
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	If a CN value ~~is given~~ that is dependent on the soil type and land use (see /DVWK, 1991/), ~~a prehistoric~~ initial ~~loss as well as~~ a ~~prehistoric~~ relationship of the runoff coefficient ~~from~~ the amount ~~of precipitation accumulated~~ up to the time ~~under consideration~~ can be ~~formulated~~ /Zaiss, 1987/~~; i.e~~. the runoff coefficient increases with increasing precipitation in the course of the event.		Using a CN value that is dependent on the soil type and land use (see /DVWK, 1991/), the initial losses and a relationship between the runoff coefficient and the accumulated rainfall amount up to the current point in time can be derived, both of which are dependent on previous conditions /Zaiss, 1987/. With this approach, the runoff coefficient increases with increasing precipitation amount during the course of the rainfall event.
	The quantification of the ~~prehistory~~ is based on the 21-day-precipitation index <math>VN</math>		The quantification of the previous conditions is based on the 21-day-precipitation index <math>VN</math>.

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2020-10-08T15:21:31Z

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If a CN value is given that is dependent on the soil type and land use (see /DVWK, 1991/), a prehistoric initial loss as well as a prehistoric relationship of the runoff coefficient from the amount of precipitation accumulated up to the time under consideration can be formulated /Zaiss, 1987/; i.e. the runoff coefficient increases with increasing precipitation in the course of the event.
The quantification of the prehistory is based on the 21-day-precipitation index <math>VN</math>