Diagram the ocean currents and predict which coasts have warm currents and which have cold water. 12. Describe the continental, oceanic and montane effects on climate. 13. Given a description of a mountain range and knowledge of the prevailing winds, draw a graph predicting precipitation as a function of elevation.
11. Diagram the ocean currents and predict which coasts have warm currents and which have cold water. 12. Describe the continental, oceanic and montane effects on climate. 13. Given a description of a mountain range and knowledge of the prevailing winds, draw a graph predicting precipitation as a function of elevation. Biomes
Feb 07, 2022 · Ocean Currents have an important role in changing the climate of a certain area. They affect the temperature of the nearby landmass. Warm currents that move from the equator towards the poles carry warm water. On the other hand, cold currents that travel from the poles toward the equator carry cold water. Figure 3 shows different loops or gyres ...
Coastal for montia lies next to a large body of water. Water's high specific heat means that the water can observe high levels of heat energy without raising many degrees in temperature, so helps to stabilize temperature changes in the land next to it. Further, the ocean provides a source of humidity for the air in coastal Fremontia which also stabilizes land temperatures.
What seems to determine whether a current carries warm or cold water? Currents originating in low latitudes near the equator tend to carry warmer water. Currents originating in high latitudes near the north or south pole tend to carry colder water.
Surface currents The warm Gulf Stream originating in the tropical Caribbean, for instance, carries about 150 times more water than the Amazon River. The current moves along the U.S. East Coast across the Atlantic Ocean towards Europe.Aug 1, 2011
For example, along the west coasts of the continents, the currents flow toward the equator in both hemispheres. These are called cold currents as they bring cool water from the polar regions into the tropical regions. The cold current off the west coast of the United States is called the California Current.
They are classified into three-part i.e. Drift, Current, and Stream on the basis of the direction of flow, speed, and shape. They can be cold, warm, and hot....List of Ocean Currents of the World.Name of CurrentNature of CurrentAntarctica CurrentColdOkhotsk CurrentColdFlorida CurrentWarmGulf StreamWarm30 more rows•Jan 3, 2022
As water temperatures begin to decrease and salinity increase, the water becomes denser and sinks. Then, the cold water flows back along the ocean floor as a deep current. Deep currents move and mix water around the world. They carry cold water from the poles toward the equator.
coldThe current is cold and has a low salinity; it maintains temperatures of less than 32° F (0° C) and salinities in the range of 30 to 34 parts per 1,000.
The Gulf Stream is one of the strong ocean currents that carries warm water from the tropics to the higher latitudes.
west coastThe Humboldt Current is a cold water ocean current that flows north from Antarctica along the west coast of South America, bringing nutrient rich water to the Galapagos Islands and helping to sustain the islands rich biodiversity.
The Gulf Stream is a strong ocean current that brings warm water from the Gulf of Mexico into the Atlantic Ocean. It extends all the way up the eastern coast of the United States and Canada. The Gulf Stream is a strong ocean current that brings warm water from the Gulf of Mexico into the Atlantic Ocean.
cold currentIt is a very cold current with temperatures ranging from –1 to 5°C depending on the time of the year, and with speeds up to 2 knots (3.7 km per hour). Antarctica is also the place where waters form that flow through the deep ocean as part of the global Ocean Conveyor (World Circulation).
Any current flowing from the equatorial region toward the polar region is des- ignated as warm; any current flowing from the polar region toward the equator is designated as cold.
Its northern boundary is usually near 4°N, while the southern boundary is usually found between 15-25°S, depending primarily on longitudinal location and the time of the year. The relatively cool Benguela Current flows northward to feed the southern branch of the SEC.