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rylen 3.2
| Term | Definition |
|---|---|
| water | Water is a polar molecule essential for life and many Earth processes. |
| polarity | Polarity is the uneven distribution of electrical charge in a molecule. |
| surface tension | Surface tension is the strong attraction between water molecules at the surface. |
| capillary action | Capillary action is water moving upward through narrow spaces due to cohesion and adhesion. |
| cohesion adhesion | Cohesion is water molecules sticking to each other. |
| capacity | Capacity is the ability of something to hold or store heat, energy, or matter. |
| temperature | Temperature measures how hot or cold something is based on particle motion. |
| agent | An agent is something that causes change or produces an effect. |
| climate | Climate is the long-term average weather of a region. |
| heat | |
| convection | Convection is heat transfer by the movement of fluids like air or water. |
| energy transfer | Energy transfer is the movement of energy from one place or form to another. |
| store | To store energy means to hold it for later use. |
| absorb | To absorb energy means to take it in. |
| transmit | To transmit energy means to pass it through a material or space. |
| energy | Energy is the ability to do work or cause change. |
| deep ocean | The deep ocean is cold, dense water far below the surface. |
| surface water | Surface water is the warmer, less dense water at the top of the ocean. |
| Coriolis effect | The Coriolis effect is the bending of moving air or water due to Earth’s rotation. |
| specific heat | Specific heat is how much energy a substance needs to change temperature. |
| density | Density is how much mass is packed into a given volume. |
| salinity | Salinity is the amount of salt dissolved in water. |
| current | A current is a continuous flow of water in a certain direction. |
| thermohaline circulation | Thermohaline circulation is global ocean movement driven by temperature and salinity differences. |
| ocean currents | An ocean current is a large-scale movement of seawater through the ocean. |
| wind patterns | Wind patterns are the typical directions and strengths of winds over Earth. |
| specific heat capacity | Specific heat capacity is the amount of heat needed to raise a substance’s temperature. |
| latent heat | Latent heat is energy absorbed or released during a phase change without temperature change. |
| evaporation | Evaporation is when liquid water turns into water vapor. |
| condensation | Condensation is when water vapor turns into liquid water. |
| energy circulations | Energy circulations are large-scale movements of energy through Earth’s systems. |
| thermocline | The thermocline is a layer in the ocean where temperature changes rapidly with depth. |
| halocline | The halocline is a layer where salinity changes sharply with depth. |
| melting | Melting is the change from solid to liquid. |
| freezing | Freezing is the change from liquid to solid. |
| wave formation | Wave formation happens when wind transfers energy to the surface of water. |
| heat transfer | Heat transfer is the movement of thermal energy from warmer areas to cooler ones. |
| adhesion | Adhesion is water sticking to other materials. |