Most large rivers are perennial, meaning they maintain flow throughout the year. However, many headwater streams or streams in arid regions sometimes run dry. A stream is considered temporary if surface flow ceases during dry periods. Temporary streams are often classified further as intermittent and ephemeral. An intermittent stream becomes seasonally dry when the groundwater table drops below the elevation of the streambed during dry periods. A spatially intermittent stream may maintain flow over some sections or surface water in deep pools even during dry periods due to locally elevated water tables or perched aquifers. An ephemeral stream only flows in direct response to precipitation such as thunderstorms. Thus, the flow variability of an intermittent stream is much more predictable than in an ephemeral stream.
In many parts of the world, such as the desert southwest, temporary streams may comprise a majority of the river network, >80% in some areas. However, even in wet regions, temporary streams at the head of river networks can account for >50% of the total stream network. Thus, river networks can be considered dynamic systems, with total miles of surface flow expanding and contracting in response to precipitation events.
Why would we still call a channel that goes dry for much of the year a stream? In other words, how can we distinguish between a temporary stream and an upland terrestrial ecosystem? In short, a stream has characteristic hydrological, geomorphological, and ecological processes. However, as with many topics in environmental science, the distinction between stream channels and uplands and between perennial streams and temporary streams is often fuzzy and scale-dependent. Individual stream channels may hold water for decades and then become dry during exceptional droughts that occur infrequently (once every 50-100 years). Similarly, small gullies on hillsides may flow only a few days of the year and may transport sediment but not be resident to aquatic life. Are such systems part of the river network?
A channel is generally classified as a stream based on the occurrence of several processes including Hydrological Processes, Geomorphological Processes, and Ecological Processes.
A proper stream generally consists of concentrated, channelized flow, even if it only carries water for a few days of the year. In contrast, an upland system may have surface water flow, but the flow is more akin to sheet flow and typically not concentrated into channels.
A stream channel is an area of rapid conveyance of sediment and dissolved constituents during periods of flow. However, not all sediment can be transported during all flows, and this provides a mechanism and particular pattern of sediment sorting that is a hallmark of stream channels not found in terrestrial systems.
A stream channel supports populations of aquatic organisms such as fish and insects. In contrast, upland systems do not provide even temporary habitat for aquatic organisms. Even when stream channels go dry on the surface, fish and other organisms can survive in isolated pools of water or in isolated areas of flow such as springs and perched aquifers.
Many organisms can survive in the bed of a stream channel even if the surface is dry, due to hyporheic flow, which is water that flows in the sediments of a stream channel beneath the surface.
Even if aquatic organisms do not persist in stream channels year-round, temporary flooding can provide productive systems and isolation from predators, favorable for reproduction and development of young organisms, which can then migrate to perennial rivers as the stream dries.