The Gulf Stream and the Kuroshio Current are both warm ocean currents that primarily flow away from the equator. The Gulf Stream flows from the Gulf of Mexico across the North Atlantic Ocean, while the Kuroshio Current flows along the eastern coast of Japan.
The East Australian Current flows southward along Australia's east coast in the Pacific Ocean. The Kuroshio Current flows northward along Japan's east coast in the western North Pacific Ocean.
A parallel circuit has more than one current branch. In a parallel circuit, the components are connected in separate paths to the voltage source, allowing for multiple current paths and different current levels through each branch.
The three major surface currents of the ocean are the Gulf Stream in the North Atlantic, the Kuroshio Current in the North Pacific, and the Antarctic Circumpolar Current in the Southern Ocean. These currents play a significant role in redistributing heat around the globe and influencing regional climates.
In a parallel circuit, the total amperage increases as the number of bulbs increases because the current has multiple paths to flow through. Each bulb offers a separate path that allows more current to flow. In a parallel circuit, adding more bulbs decreases the total resistance, allowing more current to pass through.
The Kuroshio Current is warm. It is a nutrient-rich warm ocean current that flows along the eastern coast of Japan.
it has a warm current
The Kuroshio Current.
it is in north pacific ocean (oceangraphy).
kuroshio current
Any relation !!
The Gulf Stream and the Kuroshio Current are both warm ocean currents that primarily flow away from the equator. The Gulf Stream flows from the Gulf of Mexico across the North Atlantic Ocean, while the Kuroshio Current flows along the eastern coast of Japan.
The East Australian Current flows southward along Australia's east coast in the Pacific Ocean. The Kuroshio Current flows northward along Japan's east coast in the western North Pacific Ocean.
A current that runs parallel to the shoreline is called a rip tide or rip current.
Current travels in loops. In series you have one loop, or path for current to take. With parallel connections, there's at least two. This is why current divides in parallel and not in series.
In a parallel circuit, the hypothesis is that when components are connected in parallel, the total current flowing into the junction equals the total current flowing out. Essentially, the hypothesis states that the total current remains constant regardless of the number of parallel paths.
by adding resistance in parallel more current is bound to flow