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Nature of Science
unit 1- very amazingz be teh scared :0
| Term | Definition |
|---|---|
| empirical evidence | |
| theory | Something based on tons of supporting evidence. Scientists make them a lot, but they change overtime based on other things. |
| law | |
| experiment | The act of using things and testing them, gathering evidence, and eventually doing it again until you get a result. |
| hypothesis | A starting guess/theory of an experiment. Basically, an idea of what will happen before you start. |
| dependent variable | A variable/thing that depends on another. |
| observation | Looking at something to study it, or to get information from it. |
| Conclusion | The ending or final result of your science experiment. |
| Inference | A logical conclusion drawn from your observations. |
| Earth system | Earth System Science is the study of the interconnected components of our environment, and how they interact to produce an integrated whole. |
| Geosphere | any of the almost spherical concentric regions of matter that make up the earth and its atmosphere, as the lithosphere and hydrosphere. |
| Hydrosphere | A hydrosphere is the total amount of water on a planet. The hydrosphere includes water that is on the surface of the planet, underground and in the air. |
| Cryosphere | the region of the earth's surface where water is in the form of ice or snow. |
| Atmosphere | the envelope of gases surrounding the earth or another planet. |
| Biosphere | the regions of the surface, atmosphere, and hydrosphere of the earth (or analogous parts of other planets) occupied by living organisms. |
| Energy budget | Earth’s energy budget represents the balance between the amount of energy incoming to Earth from the Sun and the amount of energy outgoing from Earth back to space. |
| Air pressure | Air pressure is the force or weight of air molecules pushing down on Earth's surface and everything it touches. |
| Thermosphere | the region of the atmosphere above the mesosphere and below the height at which the atmosphere ceases to have the properties of a continuous medium. The thermosphere is characterized throughout by an increase in temperature with height. |
| Mesosphere | the region of the earth's atmosphere above the stratosphere and below the thermosphere, between about 30 and 50 miles (50 and 80 km) in altitude. |
| Stratosphere | the layer of the earth's atmosphere above the troposphere, extending to about 32 miles (50 km) above the earth's surface (the lower boundary of the mesosphere). |
| Troposphere | the lowest region of the atmosphere, extending from the earth's surface to a height of about 3.7–6.2 miles (6–10 km), which is the lower boundary of the stratosphere. |
| Ozone layer | a layer in the earth's stratosphere at an altitude of about 6.2 miles (10 km) containing a high concentration of ozone, which absorbs most of the ultraviolet radiation reaching the earth from the sun. |
| Greenhouse effect | the trapping of the sun's warmth in a planet's lower atmosphere, due to the greater transparency of the atmosphere to visible radiation from the sun than to infrared radiation emitted from the planet's surface. |
| Temperature | In science, temperature is a measure of the average speed and energy of the tiny moving particles (atoms and molecules) that make up an object. |
| Thermal energy | Thermal energy is the total internal energy produced by the microscopic, random movement and vibration of atoms and molecules within a substance. |
| Heat | heat is the transfer of thermal energy from one object or system to another due to a difference in temperature. |
| Radiation | radiation is the emission or transmission of energy in the form of waves or particles through space or through a material medium. |
| Convection | Convection is the transfer of heat through the movement of heated fluids like liquids or gases. |
| Conduction | Conduction in science is the transfer of thermal or electrical energy through direct physical contact between particles of matter, without the overall movement of the matter itself. |
| Wind | wind is the large-scale movement of air or other gases relative to a planet's surface, flowing horizontally from areas of high pressure to areas of low pressure. |
| Coriolis effect | The Coriolis effect is an apparent curving path of objects moving long distances over the Earth, caused by the planet's rotation. |
| Global winds | Global winds are large-scale patterns of air circulation that move across the Earth's surface in steady, predictable directions. |
| Jet stream | A jet stream is a fast, narrow current of strong winds flowing from west to east high in the Earth's atmosphere. |
| Local winds | Local winds are winds that blow over a limited area. Local winds blow between small low and high pressure systems. |
| Ocean wind | An ocean current is a continuous, directed movement of seawater generated by forces like wind, the Earth's rotation, and water density differences. |
| Surface current | A surface current is a continuous, directed movement of ocean water in the upper layer of the water column, primarily driven by global wind friction. |
| Deep current | Deep ocean currents, characterized by both vertical and horizontal movements of seawater, play a crucial role in the global ocean system. |
| Convection current | A convection current is a continuous circular pattern of fluid movement driven by differences in temperature and density. |
| Upwelling | Upwelling is an oceanographic process where strong winds and the Earth's rotation push warm surface water away, allowing cold, nutrient-dense water from the deep ocean to rise to the surface. |