On the outer bank (at the tip of the meander)
Jet streams are fast flowing, narrow, meandering air currents in the atmospheres of some planets, including Earth. On Earth, the main jet streams are located near the altitude of the tropopause and are westerly winds (flowing west to east).
The age of a stream can be estimated by examining its characteristics and features. Younger streams typically have steep, V-shaped valleys, a straight path, and a lack of sediment deposits. In contrast, older streams often exhibit wider, more meandering channels, flatter valleys, and well-developed floodplains with significant sediment accumulation. Additionally, the presence of certain geological formations and the degree of erosion can provide clues about the stream's age.
Jet streams originate from the combination of the Earth's rotation and the uneven heating of its surface by the sun. These fast-flowing air currents form at the boundaries of different air masses, particularly between polar and tropical regions, where temperature gradients are strongest. The Coriolis effect, resulting from the Earth's rotation, helps shape and direct these streams. Jet streams typically occur in the upper levels of the atmosphere, influencing weather patterns and systems.
desert streams get flash floods more than the streams in the humid places.
Streams of Expression was created on 2005-12-13.
The physical feature that is commonly described as meandering or braided are streams or rivers. Braided streams are fast moving waters in multiple shallow channels. Meandering streams are single streams on gently sloped or flat areas.
meandering
Meandering streams have a sinuous, sweeping pattern with curves and bends, while meandering valleys are wide and gently sloping. They often have a well-developed floodplain and abundant vegetation along the banks. Meandering streams and valleys typically form in areas with soft, easily eroded sediment.
Meandering streams have a sinuous flow pattern with curves and bends, while meandering valleys have a gently sloping, winding shape. Meandering streams often erode the outer banks and deposit sediment on the inner banks, creating point bars. Both streams and valleys develop distinct cutbanks and point bars as water moves along the meandering path.
Meandering streams are commonly found in gently sloping landscapes where the water flow is slow and the stream has the ability to erode the banks and create curves. They are often seen in plains, valleys, and floodplains.
Close to the base level.
How would YOU know there's a meandering stream of air 30,000 feet above you
Such valleys are typically formed by sediments carried and deposited by meandering streams over time. The slow and lateral movement of meandering streams creates a wide, flat valley floor as they continuously deposit sediment along their banks. These types of valleys can often be found in regions with low gradients and high sediment loads.
Meandering and braided are terms commonly used to describe types of rivers or streams.
Jet streams are fast flowing, narrow, meandering air currents in the atmospheres of some planets, including Earth. On Earth, the main jet streams are located near the altitude of the tropopause and are westerly winds (flowing west to east).
Jet streams are fast flowing, narrow, meandering air currents in the atmospheres of some planets, including Earth. On Earth, the main jet streams are located near the altitude of the tropopause and are westerly winds (flowing west to east).
They occur at the boundaries between the first, second, and third wind systems