The Gulf Stream is a warm ocean current that originates in the Gulf of Mexico and flows northward along the eastern coast of the United States, significantly influencing the climate of the Atlantic region. In contrast, the California Current is a cold ocean current that flows southward along the western coast of North America, bringing cooler temperatures to the coastal areas of California and the Pacific Northwest. These two currents differ in temperature, origin, and their effects on regional climates. Additionally, the Gulf Stream is part of the Atlantic Meridional Overturning Circulation, while the California Current is part of the North Pacific Gyre.
southern equatorial current
The main difference between stream pools and ponds is that stream pools are dynamic water bodies formed in the current of a flowing stream, where water collects and slows down, often creating deeper areas. In contrast, ponds are typically still water bodies that can be isolated from flowing water systems. Stream pools are influenced by the flow of the stream, while ponds are more stable and can support distinct ecosystems.
The Gulf Stream and the California current are the two ocean currents that affect North America. The California current originates in the Pacific Ocean, while the Gulf Stream originates in the Atlantic Ocean.
warmer towards california and colder towards england
a ocean current between America and England
Voltage is the number of electrons relative to another location; current is how many of those electrons are moving from one location to another. A simple example is a stream. Think of voltage as the width and depth of the stream, and current as how fast the stream is moving. If it is very big, but not moving, it is not very dangerous. Alternatively, if it is very small and moving quickly it is not really dangerous. But if it is big and moving quickly, it becomes dangerous.
A continental jet-stream travels parallel to the equator - a polar jet-stream travels in a north/south direction.
Gulf Stream
Speeds up
They are complimentary the gulf stream caries warm surface waters north. The north equatorial current carries cold deep waters south.
A fast flowing river is faster
difference between the high flood level and stream bed datum.