17 3earth Vocab
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This document discusses key concepts related to temperature controls. It defines albedo as the reflection of total radiation from a surface and isotherm as a line connecting equal temperature points. It also notes that in addition to latitude, factors like land/water heating, altitude, position, cloud cover, and ocean currents strongly influence temperature, with land heating and cooling more rapidly than water.
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This document discusses key concepts relating to temperature controls. It explains that factors beyond latitude like heating of land vs water, altitude, geographic position, cloud cover and ocean currents strongly influence temperature. Land heats and cools more rapidly than water. Many clouds have a high albedo and reflect sunlight back to space rather than allowing it to heat the surface.
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2. The Earth is heated through radiation from the sun, with some energy being absorbed, some reflected, and some transmitted through substances like water and air.
3. Temperatures vary based on factors like proximity to water vs. land, altitude, latitude, and cloud cover, with land experiencing greater temperature ranges than water and higher latitudes being cooler on average.
Air pressure
Air pressure is exerted equally in all directions by the air around us. It can be measured using a barometer, with units of mmHg or atm. Rapid changes in air pressure often indicate approaching weather systems - falling pressure means storms while rising pressure means clearing weather. Winds are created by differences in air pressure between areas. Global wind patterns are caused by uneven heating of the Earth, with the hottest air at the equator rising and causing circulation of air masses. High and low pressure systems form based on temperature and moisture levels, influencing wind direction.
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This document discusses factors that influence temperature variations from place to place and time to time. It explains that temperature is affected by factors like latitude, proximity to water or land, altitude, cloud cover, ocean currents, and albedo. Land heats and cools faster than water, and the Northern Hemisphere has less water than the Southern Hemisphere. Geographic position, cloud cover, altitude also impact temperatures. Near the equator is hotter while near the poles is cooler due to differences in solar radiation by latitude.
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This document discusses various factors that influence global and local temperatures, including:
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- Outgoing longwave radiation is absorbed by greenhouse gases, contributing to the greenhouse effect.
- Ocean currents and atmospheric winds transfer heat energy from the equator toward the poles.
- Latent heat transport through evaporation and condensation also helps regulate global temperatures.
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This document discusses factors that influence temperature variations from place to place and time to time. It explains that temperature is affected by factors like latitude, proximity to water or land, altitude, cloud cover, ocean currents, and albedo. Land heats and cools faster than water, and the Northern Hemisphere has less water than the Southern Hemisphere. Geographic position, cloud cover, altitude also impact temperatures. Near the equator is hotter while near the poles is cooler due to differences in solar radiation by latitude.
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- Ocean currents and atmospheric winds transfer heat energy from the equator toward the poles.
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There are many factors that influence temperature variations from place to place and time to time. Land heats and cools more rapidly than water, causing larger temperature changes over land. Altitude also affects temperature, with higher altitudes experiencing cooler temperatures. The extent of cloud cover impacts temperatures by reducing incoming solar radiation on cloudy days but trapping heat at night. Geographic features like proximity to bodies of water or position relative to the equator further influence local temperatures.
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Wind shapes landscapes through processes like deflation, desert pavement formation, and loess and dune deposition. Deflation is the lifting and removal of loose material by wind. Desert pavement is a layer of coarse pebbles created when wind removes finer material. Loess deposits are windblown silt deposits that form blanket-like layers, while dunes are ridges of wind-deposited sand that can vary in shape depending on wind and vegetation factors.
Earth science 7.2
Much of the weathered debris in deserts comes from mechanical weathering like alluvial fans formed where stream slopes abruptly decrease. While chemical weathering is less common, over long periods clays and thin soils can form. Desert streams are ephemeral, only flowing after rain, and often drying up before reaching oceans due to evaporation and soil infiltration. Most desert erosion comes from running water, though wind also erodes deserts, water does the most erosional work.
Earth science 7.1
Glaciers are large masses of ice that originate on land from compacted snow and move due to gravity. During an ice age, large ice sheets form on continents and flow outward, carving U-shaped valleys and depositing unsorted sediment called till. Valley glaciers are smaller glaciers confined to mountain valleys that flow due to plastic deformation and basal sliding between the ice and bedrock.
Earth science 6.3
Groundwater exists below the surface in the saturated zone where all spaces between rock and sediment are filled with water. The water table marks the top of this zone, and groundwater moves slowly through porous and permeable materials. Springs form where the water table intersects the surface, and overuse or contamination can threaten groundwater supplies in some areas. Karst regions have irregular terrain with sinkholes caused by erosion of soluble rock by groundwater in caverns below the water table.
Earth science 6.2
This document defines key terms related to streams and their processes, including bed load, capacity, alluvium, delta, natural levee, floodplain, flood, drainage basin, divide. It also describes concepts such as how streams erode and deposit sediment according to flow velocities, and how flooding occurs and can be mitigated. The overall work of streams is to shape the landscape through erosion, transportation, and deposition of sediment within drainage basins.
Earth science 6.1
The document discusses key concepts about running water and the water cycle. It defines terms like infiltration, transpiration, gradient, stream channel, discharge, tributary, base level, and meander. It explains that water constantly circulates among the oceans, atmosphere, geosphere, and biosphere in the water cycle. Balance in the cycle means annual precipitation equals evaporation globally. A stream's ability to erode and transport materials depends on its velocity, while gradient decreases and discharge increases from headwaters to the mouth.
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17 3earth Vocab
- 2. Albedo Albedo is the refraction of total radiation that is reflected back by a surface.
- 3. Isotherm Isotherm is a line connecting points of equal temperature.
- 4. Factors other than latitude that exert a strong influence on temperature include heating of land and water, altitude, geographic position, cloud cover, and ocean currents.
- 5. Land heats more rapidly and to higher temperatures than water. Land also cools more rapidly and to lower temperatures than water.
- 6. Many clouds have a high albedo, and therefore reflect a significant portion of the sunlight that strikes them back to space.