Quiz 2 Flashcards

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1
Q

What is specific heat? How is it important to heating and cooling of continents and oceans

A

Specific heat is the amount of energy needed to increase a kilogram mass of a substance by 1 degree C. Because the specific heat of water is higher than that of land it takes more energy to heat the oceans than it does the land. This means that the oceans help contribute to balancing out the high heat of the land to help balance the temperatures around the world

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2
Q

What is an isotherm on a map portraying temperatures

A

An isotherm is a line that connects areas of the same temperatures.

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3
Q

Discuss how mean daily temperatures varies with increasing elevation.

A

As the elevation increases the temperature will decrease because there is less air pressure than at lower altitudes.

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4
Q

Why do temperatures vary little through the year in ushiana Argentina despite its high latitude

A

The water that surrounds the city helps to keep the temperatures moderate because water has a higher specific heat than land.

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5
Q

Discuss how high surface temperatures create low atmospheric pressure at the surface

A

High surface temperatures means that the air molecules are moving faster. This increases the volume of the gases and decreases the pressure.

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6
Q

What does an aneroid barometer measure? How does it work?

A

An Aneroid barometer measures air pressure. It works by having a evacuated chamber with a spring in it. The air pressure presses down on that spring and then through a series of pivot points an arrow points to the amount of pressure in the atmosphere.

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7
Q

What is the cause of dynamically induced surface high pressure

A

Dynamically induced surface high pressure is created by air in the upper troposphere compressing together and being forced downward.

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8
Q

Explain why a land breeze frequently develops along the coast at night

A

At night the temperature of the land has increased over the day creating high pressure and the pressure over the water is lower than that of the land. and because air moves from high to low pressure there is a land breeze over the ocean at night

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9
Q

Briefly Why is a Chinook wind warm

A

The Chinook wind is warm because as air descends from the side of the mountain it is compressed and dried out from the release of the latent heat on the other side, and as it spreads out the warm air blows across the adjacent lowland.

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10
Q

What causes the Santa Ana winds in California

A

The high pressure over the Mojave desert causes the Santa Ana winds

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11
Q

Why are polar highs more intense over land in winter than over the oceans

A

The cold dense air ove rth epoles produces high pressure and because the area already has a large energy deficit, and the continents loose energy faster than the oceans there is more high pressure over the land than there is the water

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12
Q

why are subtropical high pressure areas more intens over the oceans than over the continents

A

because the oceans are normally cooler than the continent the air warms up less over the water than the continent which means the pressure over land is lower than the pressure over land

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13
Q

How does air move at the surface in to low pressure system sin the northern hemisphere and middle latitudes? What happens to the air at the surface as it reaches the low pressure center

A

because the earth rotates air enters the low pressure areas in a counter clockwise pattern called a cyclone a the surface as it reaches the low pressure center the winds are very strong.

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14
Q

What iniciates or causes a hadley cell of air circulationin the Tropices

A

The high rising heat at the equator, and the low pressure created by this cause the hadley cells to develop.

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15
Q

Contrast the westerlies with the trade winds in two ways

A

x

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16
Q

Contrast the causes for high summer precipitation and low winter precipitation at Kolkata India

A

High precipitation in the summer is a result of moist air coming off of the oceans where as diring the dry season relfects the flow of dry air from the land flowing outward

17
Q

Breifly why does the amount of precipitation over the entire earth average 39 inches per year yet there is only one inch of precipitable water vapor in the atmosphere at any given time

A

Because of the water constatntly evaporating and condensing ni a cycle all year long

18
Q

Discuss one property of wanter that si a consequencs of its polar structure profive an exam ple that demonstrates the property you discussed above

A

Water has a capillary action which allows it to travel upward in very small places. An example of this is if you set the edge of a paper towel in a bucket of water. The water will gradually move upward through the paper towel even though the only thing touching the water is the edge

19
Q

How does the fact that water gets less dense just before it freezes affect the climate of the earth

A

Because ice is less dense than water this means it affects the climate of the earth because the oceans would freeze completely not just at the surface the earth would probably be much colder than it is now

20
Q

Why do geographers especially like specific humidity as ameasure of atmospheric water vapor content

A

Geographers like it because it is simple in the fact that it doesn’t account for changes in temperature it is jusst mass of water vapor divided by the mass of air

21
Q

Why di air parcels always cool adibatically

A

because as air moves up in the atmosphere the molecules spread out causing a decrease in temperature

22
Q

Why does the Saturated adibatic Lapse rate actually vary with temperature although we use an average value

A

because at higher temperatures the air can absorb more water than at lower temperatures

23
Q

Why is the Saturated Adiabatic Lapse rate of cooling in a rising air parcel alowasy less the the unsaturated adiabatic rate in a cooling parcel

A

Because the SALR has water vapor molecules that release latent heat which counteracts the cooling that occurs during the adibatic assent

24
Q

What is the environmental lapse Rate a measure of

A

the Environmental lapser rate is the rate of temperatrue change in the air surrounding a rising air parcel