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Sofia Colon EES 3.2
| Term | Definition |
|---|---|
| Water | a molecule (H₂O) essential for life, able to absorb, store, and transfer heat and energy. |
| Polarity | uneven charge distribution in a molecule (water has a positive and negative side). |
| Cohesion | attraction between molecules of the same substance (water sticks to water). |
| Adhesion | attraction between different substances (water sticks to other surfaces). |
| Surface tension | the “skin” on water’s surface caused by cohesion. |
| Capillary action | water’s ability to move upward through small spaces due to cohesion and adhesion. |
| Density | mass per unit volume; colder or saltier water is denser. |
| Salinity | amount of dissolved salt in water. |
| Specific heat | how much energy is needed to change a substance’s temperature. |
| Specific heat capacity | water’s ability to absorb a lot of heat with little temperature change. |
| Latent heat | energy absorbed or released during phase change (melting, freezing, evaporation). |
| Temperature | measure of average molecular motion. |
| Heat | thermal energy that moves from warmer to cooler objects. |
| Energy | the ability to do work or cause change. |
| Energy transfer | movement of energy from one place or form to another. |
| Store | to hold energy for later use. |
| Absorb | to take in energy. |
| Transmit | to pass energy through a material. |
| Heat transfer | movement of heat by conduction, convection, or radiation. |
| Melting | solid → liquid. |
| Freezing | liquid → solid. |
| Evaporation | liquid → gas. |
| Condensation | gas → liquid. |
| Surface water | warm, less dense top layer of the ocean. |
| Deep ocean | cold, dense bottom layer of the ocean. |
| Thermocline | layer where temperature changes rapidly with depth. |
| Halocline | layer where salinity changes rapidly with depth. |
| Current | continuous movement of ocean water in a direction. |
| Ocean current | large-scale flow of ocean water driven by wind, density, and Earth’s rotation. |
| Thermohaline circulation | global ocean circulation driven by temperature and salinity differences. |
| Energy circulation | movement of heat energy through the ocean and atmosphere. |
| Wind patterns | large-scale movement of air that helps drive ocean surface currents |
| Coriolis effect | deflection of moving objects due to Earth’s rotation. |
| Convection | transfer of heat by movement of fluids (warm rises, cool sinks). |
| Wave formation | waves form when wind transfers energy to surface water. |
| Agent | something that causes change (ex: water is an agent of erosion). |
| Climate | long-term average weather patterns of a region. |
| Capacity | ability to hold or store something (like heat capacity). |