Entrée : Débit des cours d'eau - montrer la version 4
URI: https://terra-vocabulary.org/ncl/DataTerraRepositoryFairIncubator/motsClefs/c_24c85133
[Wikipedia] Streamflow, or channel runoff, is the flow of water in streams, rivers, and other channels, and is a major element of the water cycle. It is one component of the runoff of water from the land to waterbodies, the other component being surface runoff. Water flowing in channels comes from surface runoff from adjacent hillslopes, from groundwater flow out of the ground, and from water discharged from pipes. The discharge of water flowing in a channel is measured using stream gauges or can be estimated by the Manning equation. The record of flow over time is called a hydrograph. Flooding occurs when the volume of water exceeds the capacity of the channel.
Métadonnées principales
| est un | Concept | feature of interest |
| modifié le | 17 Nov 2023 08:31:48.821 |
| soumis par | Hélène Bressan |
| accepté le | 22 May 2023 14:58:12.231 |
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| date accepted |
22 May 2023 14:58:12.231
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| date submitted |
22 May 2023 13:21:09.438
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| definition |
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| description |
[Wikipedia] Streamflow, or channel runoff, is the flow of water in streams, rivers, and other channels, and is a major element of the water cycle. It is one component of the runoff of water from the land to waterbodies, the other component being surface runoff. Water flowing in channels comes from surface runoff from adjacent hillslopes, from groundwater flow out of the ground, and from water discharged from pipes. The discharge of water flowing in a channel is measured using stream gauges or can be estimated by the Manning equation. The record of flow over time is called a hydrograph. Flooding occurs when the volume of water exceeds the capacity of the channel.
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feature of interest
| Concept
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| modified |
17 Nov 2023 08:31:48.821
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| notation |
c_24c85133
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| register |
mots clefs
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| status |
status experimental
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| type |
register item
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| version info |
4
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Définition
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| description |
[Wikipedia] Streamflow, or channel runoff, is the flow of water in streams, rivers, and other channels, and is a major element of the water cycle. It is one component of the runoff of water from the land to waterbodies, the other component being surface runoff. Water flowing in channels comes from surface runoff from adjacent hillslopes, from groundwater flow out of the ground, and from water discharged from pipes. The discharge of water flowing in a channel is measured using stream gauges or can be estimated by the Manning equation. The record of flow over time is called a hydrograph. Flooding occurs when the volume of water exceeds the capacity of the channel.
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| exact match |
21302
| c 24c85133
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| in scheme |
Vocabulaire des mots clefs
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| pref label |
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| same as |
c 24c85133
| 21302
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| top concept of |
Vocabulaire des mots clefs
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| type |
Concept
| feature of interest
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| was attributed to |
Pôle THEIA
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