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Project
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Description
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Pond1
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Atmospheric boundary with the high precipitation rate exceeding the soil infiltration capacity and causing the surface runoff.
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Pond2
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Atmospheric boundary with the high precipitation rate exceeding the soil infiltration capacity and resulting in the development of the surface water layer, thickness of which is not limited.
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Pond3
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Atmospheric boundary with the high precipitation rate exceeding the soil infiltration capacity and resulting in the development of the surface water layer, thickness of which is limited. Once the limit is reached, surface runoff starts.
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Pond4
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Atmospheric boundary with multiple pulses of precipitation exceeding the soil infiltration capacity and resulting in the development of the surface water layer, thickness of which is not limited.
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Pond5
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Infiltration from the surface water layer that was initially at the soil surface.
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Snow
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Simple example demonstrating the use of the "Snow" option, i.e., that precipitation water is stored as a snow layer when air temperatures are below zero. Once air temperatures are above zero, a snow layer melts (using a degree day concept). 20 cm of water is initially stored in the snow layer. Download the Hydrus project.
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