the ocean absorbs more than 50% of the heat that reaches the earths surface from the sun. The heat radiates of the ocean and makes surroundoing areas warm. but also like plants the ocean also takes in carbon dioxide out of the atmosphere which allows for the global temperature to decrease. these 2 main patterns help to keep the temprature of the earth stable.
The relationship between the temperature of the ground and its depth is that the temperature of the ground decreases as you go deeper into the Earth. This is because the deeper you go, the less influenced the ground is by surface temperature changes and the more it is affected by the Earth's internal heat.
The relationship between underground temperature and depth is that the temperature increases as you go deeper underground. This is because the Earth's core is hot, and heat is transferred from the core to the surface.
The relationship between temperature and depth underground is that the temperature generally increases as you go deeper underground. This is because the Earth's interior is hot, and the heat from the Earth's core gradually warms up the surrounding rock and soil as you move deeper underground.
The relationship between ground temperature and depth is that the temperature of the ground generally decreases as you go deeper into the Earth. This is because the deeper you go, the less influence surface conditions have on the temperature, and the ground is able to retain heat more effectively.
Wind refers to the movement of air in the atmosphere, while currents refer to the movement of water in the ocean. Wind is generated by temperature and pressure differences in the atmosphere, while ocean currents are influenced by factors such as temperature, salinity, and the Earth's rotation. Both wind and currents play important roles in shaping weather patterns and distributing heat around the Earth.
ocean currents and temperature
Which best explains the relationship between ocean currents and convection currents?(1 point) Responses Convection currents join with the Coriolis effect to create the winds that drive ocean currents. Convection currents join with the Coriolis effect to create the winds that drive ocean currents. Ocean currents rely on warm convection currents to strength the Coriolis effect. Ocean currents rely on warm convection currents to strength the Coriolis effect. Ocean currents create a Coriolis effect that increases convection currents. Ocean currents create a Coriolis effect that increases convection currents. Convection currents use the Coriolis effect to generate ocean currents.
Temperature differences between the equator and the poles drive atmospheric circulation and ocean currents, leading to the creation of weather patterns and climate zones. These differences play a key role in shaping global climate and help redistribute heat around the Earth.
Ocean currents are primarily driven by a combination of wind, temperature, salinity, and the Earth's rotation (Coriolis effect). The wind plays a significant role in creating surface currents, while differences in temperature and salinity drive deeper currents through processes like thermohaline circulation. The Coriolis effect influences the direction of ocean currents based on the Earth's rotation.
There are many different forces that create ocean currents. Among them are: the earth's rotation, salinity differences, wind, density differences, and buoyant forces. Temperature differences can create some of these differences, but we would have ocean currents even if the oceans were a uniform temperature.
Surface ocean currents are primarily driven by global winds, as the friction between the wind and the ocean's surface propels water in the direction of the wind. The Earth's rotation also influences these currents through the Coriolis effect, causing them to curve rather than flow in a straight line. This interaction creates large-scale circular patterns known as gyres in the ocean, which play a crucial role in regulating climate and distributing heat across the planet. Ultimately, the relationship between surface ocean currents and global winds is essential for maintaining the Earth's climate system.
In the atmosphere, currents are created by the uneven heating of the Earth's surface, which leads to differences in air pressure and temperature. These differences cause air to move in response, creating winds. In the hydrosphere, currents are primarily driven by winds, the Earth's rotation (Coriolis effect), and variations in water temperature and salinity.