Hydrograph limb: различия между версиями
Перейти к навигации
Перейти к поиску
Krastyn (обсуждение | вклад) (Новая страница: «A hydrograph limb is a part of a hydrograph. A typical hydrograph can be separated to baseflow and stormflow (peakflow). A peak on the hydrograph can be...») |
Krastyn (обсуждение | вклад) |
||
| (не показана 1 промежуточная версия этого же участника) | |||
| Строка 13: | Строка 13: | ||
* The '''rising limb''' of the hydrograph is the initial steep part leading up to the highest or peakflow value, mostly contributed by precipitation. | * The '''rising limb''' of the hydrograph is the initial steep part leading up to the highest or peakflow value, mostly contributed by precipitation. | ||
| − | * The '''falling (or recession) limb''' of the hydrograph is the period after the peak and is characterised by a long, slow decrease in streamflow until the baseflow is reached again<ref>Davie T. Fundamentals of Hydrology, Second Edition. – 2008</ref>. | + | * The '''falling (or recession) limb''' of the hydrograph is the period after the peak and is characterised by a long, slow decrease in streamflow until the baseflow is reached again<ref>Davie T. Fundamentals of Hydrology, Second Edition. Vol. 298. – Oxon: Routledge, 2008. – 200 p.</ref>. |
==Пример использования термина на английском языке== | ==Пример использования термина на английском языке== | ||
| − | We show that the variation in the shape of the rising limb of the annual hydrograph is controlled by variability in dust radiative forcing and surprisingly is independent of variations in winter and spring air temperatures<ref>Painter T.H., Skiles S.M.K., Deems J.S., Brandt W.T., Dozier J. Variation in Rising Limb of Colorado River Snowmelt Runoff Hydrograph Controlled by Dust Radiative Forcing in Snow // Geophysical Research Letters. – 2018.</ref>. | + | We show that the variation in the shape of the rising limb of the annual hydrograph is controlled by variability in dust radiative forcing and surprisingly is independent of variations in winter and spring air temperatures<ref>Painter T.H., Skiles S.M.K., Deems J.S., Brandt W.T., Dozier J. Variation in Rising Limb of Colorado River Snowmelt Runoff Hydrograph Controlled by Dust Radiative Forcing in Snow // Geophysical Research Letters. – 2018. – Т. 45. – № 2. – С. 797-808. </ref>. |
==Перевод использования на русском языке== | ==Перевод использования на русском языке== | ||
| − | + | Было доказано, что изменение формы ветви подъема среднегодового гидрографа вызывается изменчивостью отражающей способности снежного покрова под воздействием пыли, однако не зависит от зимней и весенней температуры воздуха. | |
==Список литературы== | ==Список литературы== | ||
<references /> | <references /> | ||
Текущая версия на 22:53, 21 декабря 2021
A hydrograph limb is a part of a hydrograph.
A typical hydrograph can be separated to baseflow and stormflow (peakflow). A peak on the hydrograph can be separated into the rising and falling limbs.
Ветвь гидрографа
Составная часть гидрографа, представленная серией последовательно увеличивающихся или уменьшающихся значений.
Восходящая ветвь называется ветвью подъема, нисходящая - ветвью спада.
Определение на английском
- The rising limb of the hydrograph is the initial steep part leading up to the highest or peakflow value, mostly contributed by precipitation.
- The falling (or recession) limb of the hydrograph is the period after the peak and is characterised by a long, slow decrease in streamflow until the baseflow is reached again[1].
Пример использования термина на английском языке
We show that the variation in the shape of the rising limb of the annual hydrograph is controlled by variability in dust radiative forcing and surprisingly is independent of variations in winter and spring air temperatures[2].
Перевод использования на русском языке
Было доказано, что изменение формы ветви подъема среднегодового гидрографа вызывается изменчивостью отражающей способности снежного покрова под воздействием пыли, однако не зависит от зимней и весенней температуры воздуха.
Список литературы
- ↑ Davie T. Fundamentals of Hydrology, Second Edition. Vol. 298. – Oxon: Routledge, 2008. – 200 p.
- ↑ Painter T.H., Skiles S.M.K., Deems J.S., Brandt W.T., Dozier J. Variation in Rising Limb of Colorado River Snowmelt Runoff Hydrograph Controlled by Dust Radiative Forcing in Snow // Geophysical Research Letters. – 2018. – Т. 45. – № 2. – С. 797-808.