An ephemeral stream is dry most of the time and ionly holds water suring and after rainfall or snowmelt events. Streams in humid climates generally have water in them at all times.
An ephemeral stream is dry most of the time and ionly holds water suring and after rainfall or snowmelt events. Streams in humid climates generally have water in them at all times.
desert streams get flash floods more than the streams in the humid places.
It holds more moisture
Homophones for "humid" include "hewed" and "hued." These words are pronounced the same as "humid" but have different meanings and spellings.
Sediments eroded from mountainsides and transported in streams are an example of the conservation of mass. The total amount of sediment that is eroded from the mountainside remains constant as it is transported by streams to other locations.
Streams are different from gullies because it doesn't dry up.
Cave passages can be humid due to water seepage from the surrounding rock layers or the presence of underground streams and rivers. The lack of ventilation in caves also contributes to high humidity levels by trapping moisture in the air.
Humid air has more water vapor mixed in it than dry air has.
Colorado has 48 different streams named Dry Creek.
Colorado has 33 different streams named Sand Creek.
Colorado has 32 different streams named Mill Creek.
The main types of streams are coldwater streams, which have cooler temperatures and support fish like trout; warmwater streams, which have higher temperatures and support fish like bass and sunfish; and transitional streams, which are influenced by tidal or anthropogenic effects. Each type of stream has unique characteristics and supports different aquatic life.