EASY 10 POiNTS TO FIRST PERSON!!!!!!!?

Question

EASY 10 POINTS TO FIRST PERSON THAT CAN GET ALL THE DEFINITIONS

convection cells --

high pressure --

low pressure --

latent heat --

evaporation --

condensation --

transpiration --

climate --

weather --

precipitation --

dew point --

specific humidity --

relative humidity --

air current --

wind --

anticyclone --

cyclone --

jet stream --

monsoon --

cold front --

warm front --

isobars --

occluded front --

stationary front --

Answer 1

I'm sorry...how is this an 'easy 10 points'?

Answer 2

........ i think we are all too lazy.

ps. do your own homeowork!!! i mean, go to dictionary.com!!! it's not that hard!!!

Answer 3

looks like you want someone to do your homework for you. sorry.

Answer 4

R U SERIOUS U LAZY ******!

Answer 5

1.A convection cell is a phenomenon of fluid dynamics which occurs in situations where there are temperature differences within a body of liquid or gas.

2.High pressure science and engineering is studying the effects of high pressure on materials and the design and construction of devices, such as a diamond anvil cell, which can create high pressure.

3. an air mass of lower pressure; often brings precipitation;

4.latent heat is the amount of energy in the form of heat released or absorbed by a substance during a change of phase (i.e. solid, liquid, or gas), – also called a phase transition.

5.Evaporation is the process by which molecules in a liquid state (e.g. water) spontaneously become gaseous (e.g. water vapor).

6.Condensation is the change of the physical state of aggregation (or simply state) of matter from gaseous phase into liquid phase.

7.Transpiration is the evaporation of water from the aerial parts of plants, especially leaves but also stems, flowers and roots.

8.Climate is the average and variations of weather in a region over long periods of time.

9.The state of the atmosphere at a given time and place, with respect to variables such as temperature, moisture, wind velocity, and barometric pressure.

10.Any form of water, such as rain, snow, sleet, or hail, that falls to the earth's surface.

11.The temperature at which air becomes saturated and produces dew.

12.Specific humidity The mass of water vapor per unit mass of air, including the water vapor (usually expressed as grams of water vapor per kilogram of air).

13.Relative humidity is a term used to describe the amount of water vapor that exists in a gaseous mixture of air and water.

14.air current - air moving (sometimes with considerable force) from an area of high pressure to an area of low pressure; "trees bent under the fierce winds"; "when there is no wind, row"; "the radioactivity was being swept upwards by the air current and out into the atmosphere"

15.Moving air, especially a natural and perceptible movement of air parallel to or along the ground.A movement of air generated artificially, as by bellows or a fan.

16.An extensive system of winds spiraling outward from a high-pressure center, circling clockwise in the Northern Hemisphere and counterclockwise in the Southern Hemisphere.

17.An atmospheric system characterized by the rapid inward circulation of air masses about a low-pressure center, usually accompanied by stormy, often destructive weather. Cyclones circulate counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere.

18.A high-speed, meandering wind current, generally moving from a westerly direction at speeds often exceeding 400 kilometers (250 miles) per hour at altitudes of 15 to 25 kilometers (10 to 15 miles).

19.A wind system that influences large climatic regions and reverses direction seasonally.

20.The leading portion of a cold atmospheric air mass moving against and eventually replacing a warm air mass.

21.A front along which an advancing mass of warm air rises over a mass of cold air.

22.Isobars are lines of equal atmospheric pressure drawn on a meteorological map. Each line passes through a pressure of a given value, provided certain rules are followed.

23.occluded front is formed during the process of cyclogenesis when a cold front overtakes a warm front.

24.a front that is not moving

Answer 6

convection cells --A convection cell is a phenomenon of fluid dynamics which occurs in situations where there are temperature differences within a body of liquid or gas.

high pressure --A high pressure area (also called a high or high-pressure) is a region where the atmospheric pressure is greater than surrounding areas. In some countries, these regions may be referred to as anticyclones

low pressure --A low pressure area, or "low", is a region where the atmospheric pressure is lower in relation to the surrounding area

latent heat --latent heat is the amount of energy in the form of heat released or absorbed by a substance during a change of phase (i.e. solid, liquid, or gas

evaporation --Evaporation is the process by which molecules in a liquid state (e.g. water) spontaneously become gaseous

condensation --Condensation is the change of the physical state of aggregation (or simply state) of matter from gaseous phase into liquid phase

transpiration --ranspiration is the evaporation of water from the aerial parts of plants, especially leaves but also stems, flowers and roots

climate --Climate is the average and variations of weather in a region over long periods of time

weather --the weather is a set of all extant phenomena in a given atmosphere at a given time

precipitation --precipitation (also known as one class of hydrometeors, which are atmospheric water phenomena) is any product of the condensation of atmospheric water vapor that is deposited on the earth's surface

dew point --he dew point or dewy is the temperature to which a given parcel of air must be cooled, at constant barometric pressure, for water vapor to condense into water

specific humidity --Specific humidity The mass of water vapor per unit mass of air, including the water vapor (usually expressed as grams of water vapor per kilogram of air).

relative humidity --Relative humidity is a term used to describe the amount of water vapor that exists in a gaseous mixture of air and water

air current --A current, in a river or stream, is the flow of water influenced by gravity as the water moves downhill to reduce its potential energy

wind --Wind is the flow of air. More generally, it is the flow of the gases which compose an atmosphere; since wind is not unique to Earth

anticyclone --n anticyclone (that is, opposite to a cyclone) is a weather phenomenon in which there is a descending movement of the air and a high pressure area over the part of the planet's surface affected by it

cyclone --a cyclone is an area of low atmospheric pressure characterized by inward spiraling winds that rotate counter clockwise in the northern hemisphere and clockwise in the southern hemisphere of the Earth

jet stream --Jet streams are fast flowing, relatively narrow air currents found in the atmosphere around 10 kilometers above the surface of the Earth

monsoon --monsoon is a seasonal prevailing wind which lasts for several months

cold front --cold front defined as the leading edge of a cooler and drier mass of air.

warm front --warm front is defined as the leading edge of an advancing mass of warm air; it separates warm air from the colder air ahead

isobars --isobars are lines of equal atmospheric pressure drawn on a meteorological map

occluded front --An occluded front is formed during the process of cyclogenesis when a cold front overtakes a warm front

stationary front --A stationary front is a boundary between two different air masses, neither of which is strong enough to replace the other

Answer 7

Dont ,worry, You see the book You get all answers.

Answer 8

!!!!!

Answer 9

convection cells -- cells that move in convection currents

high pressure -- very powerful pressure

low pressure --  low power pressure

latent heat --  heat absorbed

evaporation -- where heat takes up water and makes it dissapear

condensation -- RAIN!!

transpiration -- water goes through the roots

climate -- weather conditions in a certain region

weather -- rain,wind,heat,cold,etc.

precipitation -- water/rain

dew point -- tempurature where air cools down

specific humidity -- ratio of mass water vapor in the air

relative humidity -- amount of water vapor in the air

air current -- wind pretty much

wind -- gusts of air

anticyclone -- circulation of winds

cyclone --wind and system current

jet stream --strong winds

monsoon -- indian ocean seasonal winds

cold front -- zone seperating two air masses

warm front --transition of cold air and warm air

isobars --a line on a weather map

occluded front -- composite front formed when cold air moves in

stationary front --front between warm and cold air

Answer 10

meteorology????

Answer 11

ur weird

Answer 12

A convection cell is a phenomenon of fluid dynamics which occurs in situations where there are temperature differences within a body of liquid or gas.

A high pressure area (also called a high or high-pressure) is a region where the atmospheric pressure is greater than surrounding areas. In some countries, these regions may be referred to as anticyclones. Highs are frequently associated with light winds and subsidence. Subsidence will generally evaporate most cloud droplets after less than 500 meters by adiabatic heating. Thus, high pressure typically brings clear skies. During the day, since no clouds are present to reflect sunlight or reflected inki, there is more incoming shortwave solar radiation and temperatures are higher in the summer and lower in the winter. At night, the absence of clouds means that outgoing longwave radiation (i.e. heat energy from the surface) is not absorbed, giving cooler diurnal low temperatures in all seasons.

A low pressure area, or "low", is a region where the atmospheric pressure is lower in relation to the surrounding area. Tropical storms, extratropical cyclones, subpolar cyclones, and subarctic cyclones are called low-pressure cells.

In thermochemistry, latent heat is the amount of energy in the form of heat released or absorbed by a substance during a change of phase (i.e. solid, liquid, or gas), – also called a phase transition.[

Evaporation is the process by which molecules in a liquid state (e.g. water) spontaneously become gaseous (e.g. water vapor). It is the opposite of condensation. Generally, evaporation can be seen by the gradual disappearance of a liquid, when exposed to a significant volume of gas.

This article is about the physical phenomenon of condensation. The term of condensation is also used in chemistry see Condensation (organic chemistry) and Condensation reaction and the term condensate is also used in particle physics where it describes a particular state of matter.

Transpiration is the evaporation of water from the aerial parts of plants, especially leaves but also stems, flowers and roots. Leaf transpiration occurs through stomata, and can be thought of as a necessary "cost" associated with the opening of stomata to allow the diffusion of carbon dioxide gas from the air for photosynthesis. Transpiration also cools plants and enables mass flow of mineral nutrients and water from roots to shoots. Mass flow is caused by the decrease in hydrostatic (water) pressure in the upper parts of the plants due to the diffusion of water out of stomata into the atmosphere. Water is absorbed at the roots by osmosis, and any dissolved mineral nutrients travel with it through the xylem.

Climate is the average and variations of weather in a region over long periods of time. Climate zones can be defined using parameters such as temperature and rainfall to define desert, steppe, rain forest and polar ice cap regimes. Paleoclimatology is the study and description of ancient climates using information from both non-biotic factors such as sediments found in lake beds and ice cores, and biotic factors such as tree rings and coral. Climate models are mathematical models of past, present and future climates and can therefore be used to describe the likely patterns of future changes.

The weather is a set of all extant phenomena in a given atmosphere at a given time. It also includes interactions with the hydrosphere. The term usually refers to the activity of these phenomena over short periods (hours or days), as opposed to the term climate, which refers to the average atmospheric conditions over longer periods of time. When used without qualification, "weather" is understood to be the weather of Earth.

Precipitation may refer to:

Precipitation (meteorology), rain, sleet, hail, snow and other forms of water falling from the sky

Precipitation (chemistry), the condensation of a solid from a solution during a chemical reaction

Precipitation (horse), a Thoroughbred racehorse

Acid precipitation, a type of precipitation characterized by high acidity.

Ammonium sulfate precipitation, a method of purifying proteins

Ethanol precipitation, a method of concentrating DNA

Precipitation strengthening, a method used to strengthen malleable materials

Protein precipitation, a method of separating contaminants from biological products.

Basic precipitation, a type of precipitation characterized by high alkilinity.

The dew point or dewy is the temperature to which a given parcel of air must be cooled, at constant barometric pressure, for water vapor to condense into water. The condensed water is called dew. The dew point is a saturation point.

The term humidity can be known as very warm air in the atmousphere. The term humidity is usually taken in daily language to refer to relative humidity. Relative humidity is defined as the amount of water vapor in a sample of air compared to the maximum amount of water vapor the air can hold at any specific temperature in a form of 0 to 100%. Humidity may also be expressed as absolute humidity and specific humidity. Relative humidity is an important metric used in forecasting weather. Humidity indicates the likelihood of precipitation, dew, or fog. High humidity makes people feel hotter outside in the summer because it reduces the effectiveness of sweating to cool the body by preventing the evaporation of perspiration from the skin. This effect is calculated in a heat index table. Warm water vapor has more thermal energy than cool water vapor and therefore more of it evaporates into warm air than into cold air.

Relative humidity is a term used to describe the amount of water vapor that exists in a gaseous mixture of air and water.

current of air - air moving (sometimes with considerable force) from an area of high pressure to an area of low pressure; "trees bent under the fierce winds"; "when there is no wind, row"; "the radioactivity was being swept upwards by the air current and out into the atmosphere"

Wind is the flow of air. More generally, it is the flow of the gases which compose an atmosphere; since wind is not unique to Earth.[1]. Simply it occurs as air is heated by the sun and thus rises. Cool air then rushes in to occupy the area from which the hot air has now moved. It could be loosely classed as a convection current.

In meteorology, an anticyclone (that is, opposite to a cyclone) is a weather phenomenon in which there is a descending movement of the air and a high pressure area over the part of the planet's surface affected by it. Anticyclonic flow spirals in a clockwise direction in the Northern Hemisphere and counter-clockwise in the Southern.

In meteorology, a cyclone is an area of low atmospheric pressure characterized by inward spiraling winds that rotate counter clockwise in the northern hemisphere and clockwise in the southern hemisphere of the Earth. [1][2] The generic term covers a wide variety of meteorological phenomena. These include tropical cyclones, extratropical cyclones, and tornadoes, so meteorologists rarely use "cyclone" without additional qualification.

Jet streams are fast flowing, relatively narrow air currents found in the atmosphere around 10 kilometers above the surface of the Earth. They form at the boundaries of adjacent air masses with significant differences in temperature, such as the polar region and the warmer air to the south. The jet stream is mainly found in the tropopause, at the transition between the troposphere (where temperature decreases with height) and the stratosphere (where temperature increases with height)[

monsoon is a seasonal prevailing wind which lasts for several months. The term was first used in English in India, Bangladesh, Pakistan, and neighboring countries to refer to the big seasonal winds blowing from the Indian Ocean and Arabian Sea in the southwest bringing heavy rainfall to the region.[1] In hydrology, monsoon rainfall is considered to be that which occurs in any region that receives the majority of its rain during a particular season. This allows other regions of world such as within North America, South America. Sub-Saharan Africa, Australia and East Asia to qualify as

cold front defined as the leading edge of a cooler and drier mass of air. The air with greater density wedges under the less dense warmer air, lifting it, which can cause the formation of a narrow line of showers and thunderstorms when enough moisture is present. This upward motion causes lowered pressure along the cold front. On weather maps, the surface position of the cold front is marked with the symbol of a blue line of triangles/spikes (pips) pointing in the direction of travel. A cold front's location is at the leading edge of the temperature drop off, which in an isotherm analysis would show up as the leading edge of the isotherm gradient, and it normally lies within a sharp surface trough. Cold fronts can move up to twice as fast and produce sharper changes in weather than warm fronts. Since cold air is denser than warm air it rapidly replaces the warm air preceding the boundary. Cold fronts are usually associated with an area of low pressure, and sometimes, a warm front.

A warm front is defined as the leading edge of an advancing mass of warm air; it separates warm air from the colder air ahead. Air masses are large bodies of air with similar properties of temperature and humidity that form over source regions, and the warm air masses behind warm fronts are not only warmer but higher in humidity than the colder air preceding them. Because of a warm air mass’s higher temperature and thus lesser density, mixing between the two air masses is discouraged. Being lighter, the warm air mass is unable to displace the cooler air mass and instead is forced upward along the upper boundary of the colder air in a process known as overrunning

Answer 13

do ur own hw lil girl

Answer 14

Too much work

Answer 15

i dont undersand so here is a star for asking a confusing question??? :D

Answer 16

thats not an easy 10 pts......

Answer 17

i just took earth science but im too lazy to go get my old vocabulary sheets.   its not really that hard.

Answer 18

You lied! You said it would be an EASY 10 points!! This is not easy. This is time consuming and I don't know why anyone would do it for 10 points that don't even buy anything!

Answer 19

do your own ******* homework

just google/ dictionary.com/ wikipedia search those words, it'll take like 10seconds

Answer 20

Dictionary.com sweetie...10 points please and thank you.

You're not weird or lazy, clever because it was worth the try.  Someone may be bored enough for you. Patients

Answer 21

why would i answer that question...god created us with brain to think...go find it yourself.....

Answer 22

Looking up definitions is like the easiest thing in the world! But its not my homework lol, how can you be so lazy to not look up definitions, thats like have a test with the teachers copy in your face!

Answer 23

How about you do your homework yourself?

Hard homework questions, I understand.

But this is just laziness.

Answer 24

You could have looked up most of the answers in the time it took you to type them all out to post here. Good Lord.

Answer 25

lol.......use your science book

Ok, might as well, I have nothing better to do!! Here you go!!

EDIT::::::::

convection cell

–noun Physics. a distinct volume of circulating fluid, in a fluid medium under gravity, that is heated from below and cooled from above: usually found in large groupings.  

high-pres·sure

–adjective 1. having or involving a pressure above the normal: high-pressure steam.  

2. vigorous; persistent; aggressive: high-pressure salesmanship.  

low-pres·sure  

–adjective

1. having or involving a low or below-normal pressure, as steam or water.  

2. without vigor or persistence; not forceful or aggressive: a low-pressure campaign.  

3. quietly persuasive; subtle; indirect: a low-pressure salesman.  

latent heat

–noun Physics. heat absorbed or radiated during a change of phase at constant temperature and pressure.  

evaporation:

–noun 1. the act or process of evaporating.  

2. the state of being evaporated.  

3. Archaic. matter or the quantity of matter evaporated or passed off in vapor.  

con·den·sa·tion  

–noun

1. the act of condensing; the state of being condensed.  

2. the result of being made more compact or dense.  

3. reduction of a book, speech, statement, or the like, to a shorter or terser form; abridgment.  

4. a condensed form: Did you read the whole book or just a condensation?  

5. a condensed mass.  

6. (in nontechnical usage) condensate.  

7. the act or process of reducing a gas or vapor to a liquid or solid form.  

8. Chemistry. a reaction between two or more organic molecules leading to the formation of a larger molecule and the elimination of a simple molecule such as water or alcohol.  

9. Meteorology. the process by which atmospheric water vapor liquefies to form fog, clouds, or the like, or solidifies to form snow or hail.  

10. Psychoanalysis. the representation of two or more ideas, memories, feelings, or impulses by one word or image, as in a person's humor, accidental slips, or dreams.  

11. Physics. the relative amount by which the density of an elastic medium varies from its average value as a sound wave passes through it.  

transpiration::

noun 1. an action or instance of transpiring.  

2. Botany. the passage of water through a plant from the roots through the vascular system to the atmosphere.  

climate:

–noun 1. the composite or generally prevailing weather conditions of a region, as temperature, air pressure, humidity, precipitation, sunshine, cloudiness, and winds, throughout the year, averaged over a series of years.  

2. a region or area characterized by a given climate: to move to a warm climate.  

3. the prevailing attitudes, standards, or environmental conditions of a group, period, or place: a climate of political unrest.  

weather:::

–noun 1. the state of the atmosphere with respect to wind, temperature, cloudiness, moisture, pressure, etc.  

2. a strong wind or storm or strong winds and storms collectively: We've had some real weather this spring.  

3. a weathercast: The radio announcer will read the weather right after the commercial.  

4. Usually, weathers. changes or vicissitudes in one's lot or fortunes: She remained a good friend in all weathers.  

–verb (used with object) 5. to expose to the weather; dry, season, or otherwise affect by exposure to the air or atmosphere: to weather lumber before marketing it.  

6. to discolor, disintegrate, or affect injuriously, as by the effects of weather: These crumbling stones have been weathered by the centuries.  

7. to bear up against and come safely through (a storm, danger, trouble, etc.): to weather a severe illness.  

8. Nautical. (of a ship, mariner, etc.) to pass or sail to the windward of: to weather a cape.  

9. Architecture. to cause to slope, so as to shed water.  

–verb (used without object) 10. to undergo change, esp. discoloration or disintegration, as the result of exposure to atmospheric conditions.  

11. to endure or resist exposure to the weather: a coat that weathers well.  

12. to go or come safely through a storm, danger, trouble, etc. (usually fol. by through): It was a difficult time for her, but she weathered through beautifully.  

—Idiom13. under the weather, Informal. a. somewhat indisposed; ailing; ill.  

b. suffering from a hangover.  

c. more or less drunk: Many fatal accidents are caused by drivers who are under the weather.  



precipitation:::

. Meteorology. a. falling products of condensation in the atmosphere, as rain, snow, or hail.  

b. the amount of rain, snow, hail, etc., that has fallen at a given place within a given period, usually expressed in inches or centimeters of water.



dew point::::

the temperature to which air must be cooled, at a given pressure and water-vapor content, for it to reach saturation; the temperature at which dew begins to form.  

Also called dew-point temperature.

specific humidity:::::

–noun the ratio of the mass of water vapor in air to the total mass of the mixture of air and water vapor.  

relative humidity:::::

–noun the amount of water vapor in the air, expressed as a percentage of the maximum amount that the air could hold at the given temperature; the ratio of the actual water vapor pressure to the saturation vapor pressure.  

air current:::::

noun

air moving (sometimes with considerable force) from an area of high pressure to an area of low pressure; "trees bent under the fierce winds"; "when there is no wind, row"; "the radioactivity was being swept upwards by the air current and out into the atmosphere"

wind::::

1. air in natural motion, as that moving horizontally at any velocity along the earth's surface: A gentle wind blew through the valley. High winds were forecast.  

anticyclone::::

–noun Meteorology. a circulation of winds around a central region of high atmospheric pressure, clockwise in the Northern Hemisphere, counterclockwise in the Southern Hemisphere.

cyclone::::

–noun 1. a large-scale, atmospheric wind-and-pressure system characterized by low pressure at its center and by circular wind motion, counterclockwise in the Northern Hemisphere, clockwise in the Southern Hemisphere

jet stream::::

–noun 1. strong, generally westerly winds concentrated in a relatively narrow and shallow stream in the upper troposphere of the earth.  

monsoon:::::

noun 1. the seasonal wind of the Indian Ocean and southern Asia, blowing from the southwest in summer and from the northeast in winter.  

cold front::::

noun the zone separating two air masses, of which the cooler, denser mass is advancing and replacing the warmer.  

warm front:::::

noun Meteorology. a transition zone between a mass of warm air and the colder air it is replacing

isobars:::::

A line on a weather map connecting points of equal atmospheric pressure. Also called isopiestic.

occluded front:::::

noun Meteorology. a composite front formed when a cold front overtakes a warm front and forces it aloft.  

stationary front:::::

noun Meteorology. a front between warm and cold air masses that is moving very slowly or not at all.