Chapter 6 Flashcards

(45 cards)

1
Q

Heat

A

energy in the process of being transferred from one object to another because of the temperature difference between them. In the atmosphere, heat is commonly transferred by conduction, convection, advection, and radiation.

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2
Q

Radiation

A

The emission of energy from an object in the form of electromagnetic waves and photons.

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3
Q

Absorption

A

(1) Process of taking in and being made part of an existing quantity of matter. (2) Interception of electromagnetic radiation or sound.

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4
Q

Emission

A

(1) The process where an object releases energy in the form of a photon into its surrounding environment. This process produces electromagnetic radiation. (2) The creation and release of something into the surrounding environment.

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5
Q

Insolation

A

Direct and diffused shortwave solar radiation that is received in the Earth’s atmosphere or at its surface.

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6
Q

Long wave radiation

A

A form of electromagnetic radiation with a wavelength roughly between 0.7 and 100 micrometers (μm). Also called infrared radiation.

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7
Q

Greenhouse effect

A

causes the atmosphere to trap more heat energy at the Earth’s surface and within the atmosphere by absorbing and remitting longwave energy. Of the longwave energy emitted back to space, 90% is intercepted and absorbed by greenhouse gases.

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8
Q

Net radiation

A

Balance between incoming and outgoing shortwave and longwave radiations.

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9
Q

Thermometer

A

Device used to measure temperature]

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10
Q

Liquid in glass thermometer

A
  • A thermometer design that uses a thermally sensitive liquid incased in a graduated clear glass container. Changes in temperature cause the liquid to either expand (warming of temperature) or contract (cooling of temperature). The most commonly used liquids for this type of instrument are mercury and alcohol. Used for air temperature.
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11
Q

Heat energy

A

A form of energy created by the combined internal motion of atoms in a substance.

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12
Q

Fahrenheit scale

A

Scale used in the measurement of temperature. In this scale, water boils at 212° and freezes at 32 deg

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13
Q

Minimum thermometers

A

A meteorological thermometer designed to record the minimum temperature over a set time interval, usually 24 hours (midnight to midnight). Liquid-in-glass type of minimum thermometers are normally filled with red colored alcohol and have a black metal slider that can move up and down through the bore. When temperature drops, the black metal slider is pushed by the retreating top surface of the alcohol because of surface tension down the bore. When temperature begins to rise again the slider is designed not move thereby permanently recording the minimum temperature. The slider is reset by positioning the thermometer upside down.

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14
Q

Maximum thermometer

A

A meteorological thermometer designed to record the maximum temperature over a set time interval, usually 24 hours (midnight to midnight). Liquid-in-glass type of maximum thermometers have a bore that is narrowed between the reserve bulb and graduated portion of the glass stem. With rise in temperature, the mercury found in reserve bulb pushes past the constriction and up into the graduated section as long as temperature continues to increase. The mercury in the graduated section does not fall back into the reserve bulb because of the constriction and as a result the highest temperature reached is recorded.

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15
Q

Surface air temperature

A

In terms of meteorology and weather forecasting, this term refers to the temperature of the air about 1.5 meters (4.5 feet) above the ground surface where it is routinely measured at weather stations on land surfaces.

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16
Q

Stevenson screen

A

A specially designed housing for meteorological instruments used to keep measurements standardize around the world. This housing consists of wooden box painted white with double louvered sides. It is mounted on a stand 1.5 meters or 4.5 feet (this does vary from country to country between 1.2 to 1.8 meters or 3.9 to 5.9 feet) above the ground surface and contains maximum and minimum thermometers, barometer, and dry- and wet-bulb thermometers

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17
Q

Maximum Minimum Temperature System

A

Refers to a device that records maximum and minimum temperature over a period of time, usually 24 hours (midnight to midnight). MMTS are usually electronic employing a thermistor, a type of electronic resistor that is sensitive to temperature change). In a thermistor, resistance to the flow of electricity changes with temperature predictably and this change can be calibrated, measured, and recorded.

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18
Q

Thermistor

A

Is a type of electrical resistor whose resistance to electricity varies measurably with temperature. Asa result, thermistors are used for temperature sensors and and self-regulating heating elements.

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19
Q

Daily mean temperature

A

The average surface air temperature as recorded at a meteorological station fora location for a particular day. Usually, it is calculated by finding the difference between the warmest (daily maximum temperature) and coldest (daily minimum temperature) temperature recorded during a particular day and then dividing this value by 2

20
Q

Daily temperature range

A

The difference between the warmest (daily maximum temperature) and coldest (daily minimum temperature) temperatures recorded at a meteorological station during a particular day (midnight to midnight).

21
Q

Monthly mean temperature

A

The average surface temperature as recorded at a meteorological station for a specific month. Usually, it is calculated by summing all of daily mean temperatures for a particular month and then dividing this value by the number of days in that month.

22
Q

Annual mean temperature

A

The average surface temperature as recorded at a meteorological station for a location for a particular year. Usually, it is calculated by summing all of monthly mean temperatures and dividing by 12.

23
Q

Annual temperature range

A

The difference between the warmest and coldest monthly mean temperatures for a particular year.

24
Q

Meteorological normal

A

The calculated average of a measured meteorological variable, like surface air temperature, over a specified period of years. A period of 30 years is often used to determine normals.

25
Meteorological extreme
The highest and the lowest value for a meteorological variable in a specified period of observation.
26
Snow Line
Altitudinal or latitudinal limit separating zones where snow does not melt during the summer season from areas in which it does. Similar to the concept of firm limit except that it is not limited to glaciers.
27
Greenhouse gases
The gases responsible for a greenhouse effect to operate in a planet's atmosphere. On Earth, these gases include: water vapor (H2O), carbon dioxide (CO2); methane (CH4); nitrous oxide (N2O); chlorofluorocarbons (CFXClX); and tropospheric ozone (O3).
28
Cumulus
Puffy clouds with relatively flat bases. Cumulus clouds form when moist warm air bubbles vertically escape from the Earth's surface. 300 - 2000 meters
29
Cumulonimbus
A well developed vertical cloud that often has top shaped like an anvil. These clouds are very dense with condensed water and deposited ice. Weather associated with this cloud includes: strong winds; hail; lightning; tornadoes; thunder; and heavy rain. Thunderstorm clouds
30
Thunderstorm
A storm that typically ranges in size from several kilometers (several miles) to over 50 kilometers (30 miles) in diameter created by the rapid lifting of moist warm air which creates a cumulonimbus cloud. Thunderstorms can occur in isolation as a single celled storm or as a multi-celled storm arranged in a cluster or as a line of adjacent cells (called a squall line) found along or in front of a mid-latitude cyclone cold front.
31
Thermal conductivity
the ability of a substance to conduct heat. Some examples of substances with high thermal conductivities include: diamond, silver, copper, gold, aluminum, and iron. Some substances with low thermal conductivities include: gases like carbon dioxide
32
Conduction
(1) The direct transfer of heat energy from atom to atom through a substance along a temperature gradient. (2) The transfer of electrical energy from atom to atom through a substance when a difference in electrical potential exists.
33
Convection
Process that involves the transfer of mass and heat energy by means of vertical motions through a fluid substance like air or water.
34
Maritime effect
The effect that large ocean bodies have on the weather and climate of locations or regions. This effect results in a lower range in surface air temperature at both daily and annual scales.
35
Continental effect
The effect that continental surfaces have on the weather and climate of locations or regions. This effect results in a greater range in surface air temperature at both daily and annual scales. Compare with maritime effect.
36
Continentality
The tendency of terrestrial surfaces on Earth to experience more temperature variation than ocean surfaces. The main factor responsible for this fact is that the rock, soil, and sediment that makes up land has a lower specific heat than water.
37
Ocean Currents
Large scale horizontal flow of ocean water that is persistent and driven by atmospheric circulation.
38
Global circulation
Usually refers to large-scale flow of air in the troposphere. Also called planetary circulation.
39
Monsoon
A regional scale wind system that predictably change direction with the passing of the seasons. Monsoon winds blow from land to sea in the winter, and from sea to land in the summer. Summer monsoons are often accompanied with precipitation.
40
La Nina
Condition opposite of an El Niño. In a La Niña, the tropical Pacific trade winds become very strong and an abnormal accumulation of cold water occurs in the central and eastern Pacific Ocean.
41
El Nino
Name given to the occasional development of warm ocean surface waters along the coast of Ecuador and Peru. When this warming occurs the tropical Pacific trade winds weaken and the usual upwelling of cold, nutrient rich deep ocean water off the coast of Ecuador and Peru is reduced. The El Niño normally occurs around Christmas and lasts usually for a few weeks to a few months. Sometimes an extremely warm event can develop that lasts for much longer time periods.
42
Meridional heat transport
Transport of heat energy stored in the atmosphere and oceans from the equator to the poles
43
Sensible heat flux
Process where excess heat energy is transferred into the atmosphere. The process first involves the movement of heat energy from the Earth's surface to the atmosphere by conduction and convection. The heat energy then can move horizontally advection (atmospheric circulation).
44
Latent heat flux
Latent heat flux is the global movement of latent heat energy through circulations of air and water. Atmospheric circulation moves latent heat energy vertically and horizontally to cooler locations where it is condensed as rain or is deposited as snow releasing the heat energy stored within it.
45
Surface heat flux
Process where heat energy is transferred into land and ocean surfaces on the Earth. Much of this transfer takes place when solar radiation absorbed at the land or ocean surface is converted into heat energy. On land surfaces, surface heat is transferred down into the ground by conduction. Heat energy is transferred to greater depths in ocean surfaces because liquids have the ability mix by convection. Heat energy stored in ocean waters can also move quickly over large horizontal distances in a poleward direction through ocean currents.